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HomeMy WebLinkAbout20040561 Ver 4_More Info Received_20200825Strickland, Bev From: Coats, Heather Sent: Tuesday, August 25, 2020 4:55 PM To: Deaton, Anne; Harding, Kimberlee k; Mairs, Robb L; Dunn, Maria T. Cc: Smith, Ronnie D CIV USARMY CESAW (USA); MacPherson, Tara; Howell, Jonathan Subject: Add info for Village of Bald Head Island application- Frying Pan Shoals Attachments: Comment Response Letter to DCM 2020-7-28.pdf, VBHI FPS EFH 2O20-8-19.pdf Hello everyone, Please see the Village of Bald Head Island's response to comments and concerns raised by agencies regarding their application for a major modification to DCM Permit No. 91-14, which requests approval for the one-time dredging of Frying Pan Shoals as a borrow site for beach nourishment purposes. Please review the attached information and let me know if you have any questions, comments and/or whether or not the information provided satisfies your objections/concerns. Thanks in advance, Heather Heather Coats Beach & Inlet Management Project Coordinator Division of Coastal Management North Carolina Department of Environmental Quality 910 796 7302 office heather. coats(a)ncdenr.aov 127 Cardinal Drive Extension Wilmington, NC 28405 Email correspondence to and from this address is subject to the North Carolina Public Records Law and may be disclosed to third parties. LMG LAND MANAGEMENT GROUP a DiAVEY- company July 28, 2020 Ms. Heather Coats NC Division of Coastal Management Wilmington Regional Office 127 Cardinal Drive Extension Wilmington, NC 28405 RE: NC CAMA Permit Application — Major Modification Request to State Permit No. 91-14 Village of Bald Head Island Frying Pan Shoals Beach Nourishment Project Response to Request for Additional Information Dear Heather: By way of this letter and on behalf of the Village of Bald Head Island (Applicant), Land Management Group (LMG) (agent) is providing the following response to your request for additional information (RAI) dated June 26, 2020 for the Major Modification application for State Permit No. 91-14. The RAI pertained to comments received from the North Carolina Division of Marine Fisheries (DMF) by way of their letter dated June 2, 2020. Additional comments were received from the NC Wildlife Resources Commission (WRC), the NC Division of Water Resources (DWR), and the State Historic Preservation Office (SHPO). Responses to these comments are provided below (with supporting attachments where applicable and referenced). I. NC Division of Marine Fisheries Comment and Response Comment #1: DMF requests that an Environmental Impact Statement (EIS) be prepared through the USACE. Response: The Village of Bald Head Island previously as Applicant requested and participated in a project scoping meeting (conducted on October 2, 2019) at the NCDEQ Wilmington Regional Office to present the proposed action and to discuss the appropriate process for evaluating the application for a permit decision. The lead state and federal permitting agencies determined that a request to modify the Terminal Groin Individual Permit (Department of Army Permit No. SAW-2012- 00040) and the CAMA Major Permit (91-14) was the appropriate process for a permit decision. The USACE determined that an EIS is not required for this modification request. This decision was based largely on the EIS prepared for the original terminal groin permit which evaluated the use of several candidate borrow sites including the use of a borrow site on Frying Pan Shoals. In addition, an impact assessment for fishery resources is being performed as part of the updated Essential Fish Habitat (EFH) document to be submitted under separate cover. www.lmgroup.net • Phone: 910.452.0001 • Fax: 910.452.0060 3805 Wrightsville Ave., Suite 15, Wilmington, NC 28403 Page 12 Comment #2: Assess impacts to larval transport - Dredging in Frying Pan Shoals can potentially interfere with the passage of larvae and early juveniles from offshore spawning grounds into estuarine nursery areas. A detailed scientific field investigation, analysis, and modelling of larval transport dynamics that exist around Frying Pan Shoals currently and how that will change based on the proposed dredging activity. This information should be used to model estimated impacts of the dredging to larval ingress and egress through the inlet. Response: We respectfully disagree with your assessment for the potential of the dredging project to interrupt larvae and juvenile recruitment into the Cape Fear River estuary. Hydrodynamic modeling performed by Olsen for the project EIS (2014) predicted that there is no inlet -directed tidal flow on either peak ebb or peak flood conditions at Frying Pan Shoals. Therefore, there is no expected effect on the entrainment of larvae from the proposed borrow site by tidal action. The request for detailed scientific investigations of larval transport, analysis, and modeling would require a multi -year research project to be able to provide meaningful data that can control for inter -year variability. The need for such is doubtful considering that the presence of a borrow site at this location is unlikely to disrupt larval transport in any significant manner. If there is research or data in the literature indicating this phenomenon has occurred for other borrow sites, then we would respectfully request that this information or literature be shared with the Applicant so that it can be evaluated for its applicability to the proposed project. Given the size of the proposed borrow site relative to the large shoal feature (less than 0.5%) and the predicted physical recovery of the borrow area (as described further in response to Comment #3 below), it can be reasonably expected that the proposed action will not induce any large-scale disruption to circulation patterns. In addition, the excavated area will tie into natural bottom contours on the western edge of the shoal feature (i.e. there will not be a hole that could theoretically entrap or slow larvae). Rather, it is likely that vertical mixing and upwelling patterns would continue to be maintained with only limited, localized effects to currents/circulation. As a result, there is not expected to be an effect on the transport of larvae. Lastly, any assumed impacts to circulation (or disruption to upwelling) is unlikely to affect larval transport given that larvae have been demonstrated to exert considerable control over vertical movement within the water column (Morgan and Anastasia, 2008). Larvae and early juveniles are not passive in their movement. Migration of larvae outside the tidal influence of the estuary is influenced through wind -driven transport and directed vertical movement by larvae to maximize shoreward movement (Boehlert and Mundy, 1988). Once nearshore, then alongshore drift is the principal mechanism until larvae reach the entrainment influence of the estuary. Larvae are adapted to highly dynamic physical conditions in nearshore environments. Based upon the lack of any significant effects to circulation patterns, the uninterrupted wind -driven transport of larvae, the ability of larvae to exert control over vertical movement, and the large entrainment field of the Cape Fear River estuary; larval transport into the estuary will not be adversely affected. Comment #3: Assess sediment transport and refilling of borrow area - The proposal to dredge a hole, nearly 20 feet deep in some locations, in the shoal could negatively and potentially permanently alter the habitat on the shoal. Frying Pan Shoal is classified as a relict shoal receiving much of its sand deposits from the Holocene and Pleistocene periods (Normandeau Associates, Inc. 2014). These shoals formed over a long period of time and may not recover at rates necessary to www.lmgroup.net • Phone: 910.452.0001 • Fax: 910.452.0060 3805 Wrightsville Ave., Suite 15, Wilmington, NC 28403 Page 13 sustain recurring borrow activities. It is unknown how currents, wind, and storm events will respond spatially and temporally to removal of sand from the shoal. In addition, no studies have been performed to investigate the type of material that is expected to be deposited within the footprint of the excavated area. If incompatible materials fill the dredged footprint, new borrow sources will be sited on the shoal resulting in cumulative impacts to the habitat. A sediment transport model should be used to investigate the previously mentioned concerns. Response: The proposed excavation will tie into natural bottom contours along the western edge or flank of the shoal feature. As a result, there will not be a "hole" within the shoal crest. The dredge contours are designed such to induce greater rates of recharge with characteristic sand - grained sediments transported over the shoal. It is highly unlikely that there will be any fine- grained deposition post -dredging due to the ambient sediment characteristics and dynamic physical conditions of the borrow site. This is supported by observations by McNinch (2009) who commented, "Sediment dredged from the northwest flank of FPS will likely recharge episodically from sediment transported from the crest during storms, particularly extratropical nor'easters". The post -excavation substrate is expected to be self -similar to the existing condition (prior to dredging). The project as designed ensures that the depth of excavation is strategically limited such that the sediment exposed (post -dredging) has similar granular characteristics to the native seabed. In addition, the location and the design promotes rapid and continuous material transport into the excavated area. With respect to the predicted rate of sediment transport, McNinch (2009) observed the following: "The most active region of sediment recharge to FPS is likely near the cape point, particularly along the crest of the shoal where it extends seaward from the subaerial cape point and the shore parallel sand bar that merges into FPS from the updrift beach". (Note — the updrift beach or shoreline northward of the cape point is known as East Beach on BHI). Numerous individuals or organizations have performed estimates of littoral transport along the every -varying shoreline components of the State of N.C. More recently, (Van Gaalen, Tebbens and Barton, 2016) have summarized sediment transport directions from Northern Maine to Tampa Bay, FL. For the Cape Fear formation, the published rates for the two Bald Head Island shorelines that join to form the Cape Fear Point are as follows: • South Beach — 339,300 cubic meters annually toward the East. • East Beach — 341,000 cubic meters annually southward. This represents a potential net annual hypothetical rate of deposition to the Cape Fear Shoal formation of 680,300 cubic meters (i.e. 813,215 cy). Annual monitoring of South Beach indicates that net easterly transport would typically be less than that estimated above. For more information regarding sediment substrate, predicted recovery, and factors influencing borrow site selection and design, please see attached discussion prepared by Olsen Associates, Inc. (Attachment A). www.lmgroup.net • Phone: 910.452.0001 • Fax: 910.452.0060 3805 Wrightsville Ave., Suite 15, Wilmington, NC 28403 Page 14 Comment #4: DMF would also like to see the applicant explore alternative sand sources that may have less significant impacts to critical fisheries habitats; this would include previously permitted alternative borrow sources. Response: The Applicant understands and appreciates the need to explore and utilize the least environmentally damaging, practicable alternative (LEDPA) sand source site. A robust alternatives analysis of potential borrow sites was performed as part of the permit application. The only other viable site identified (of sufficient size, containing beach -quality sand, and being operationally feasible) was Jay Bird Shoals (JBS). Indeed, from a logistics standpoint there is preference to utilize the previously authorized and dredged JBS site. That being said, the Village utilized this site for a second time in its most recent Village -sponsored nourishment project (occurring in Winter 2018/2019), and Oak Island recently received authorization to dredge an approximate 304-acre borrow site located within JBS as part of a 1.1Mcy nourishment project to be implemented this coming winter (Winter 2020/21). As a result, the JBS sand resource will be depleted for the foreseeable future. However, the borrow site is continuing to be physically monitored on an annual basis. If the shoreline of South Beach can be maintained though federal nourishment for a period of time and sufficient physical recovery occurs within JBS prior to the next nourishment need, then the Village will seek to utilize JBS as an alternative sand source site prior to the use of FPS. Physical monitoring of the JBS borrow site will determine the volume of sand available for dredging prior to the next Village -sponsored nourishment, and this information will be provided to the agencies to determine if JBS can be utilized in lieu of FPS. The use of Bald Head Shoals seaward of the Point and western South Beach is not viable. Its proximity to this highly erosive section of shoreline adjacent to the federal navigation channel renders its use impracticable and counterproductive as it affords that portion of beach much needed protection through wave and current attenuation. Use of this shoal as a sand source site would result in the need for increased frequency of nourishment events, a condition not deemed environmentally favorable nor operationally and financially practicable. It can therefore be excluded from consideration as the LEDPA. Comment #5: Comments related to ecological effects of dredging within Frying Pan Shoals. Response: The Applicant will be submitting an updated Essential Fish Habitat (EFH) document with a more thorough impact assessment describing potential ecological effects to EFH habitat and managed species. A copy of this report will be submitted to both the NC DCM and NC DMF. A brief description of avoidance and minimization measures are provided below. In addition, attributes of the borrow site location and design that help to minimize ecological effects are outlined in Attachment A. The Applicant and project engineer have worked to reduce the limits of spatial impacts of the proposed borrow site based upon comments received subsequent to the submittal of the 2016 proposal. Of particular note with respect to avoidance and minimization efforts since the 2016 submittal is the following: the deletion of the dredge access corridor (aka "fairway"); the reduction in borrow site acreage (from 460.1 acres to 198.4 acres); and the limitation of dredging to an initial single borrow event to be monitored. www.lmgroup.net • Phone: 910.452.0001 • Fax: 910.452.0060 3805 Wrightsville Ave., Suite 15, Wilmington, NC 28403 Page 15 The project as designed will incorporate the following protection measures identified by the South Atlantic Fisheries Management Council (SAFMC) specific for dredge and fill projects in areas designated as Habitat Areas of Particular Concern (HAPC). These include the following: 1. Impact assessment (description of potential impacts; baseline information; alternatives analysis; construction monitoring; post -construction monitoring plan); 2. Fill material should match that of recipient beach as closely as possible; 3. Dredging to be located in areas characterized by strong currents and sand movement to promote more rapid infilling rates (and thus reducing the duration of impacts to benthic habitats); and 4. Dredging should be performed in a manner intended to minimize impacts to wave energy and currents, "thus reducing the likelihood of infilling with fine-grained sediments". In addition to the SAFMC protection measures, the proposed project incorporates following design elements that helps to further reduce or avoid impacts to natural resources: 1. The site is a highly dynamic and renewable shoal feature (maintained by seaward flow of current off cape) and thus physical and biological disturbances tend to be short-lived; 2. The position of borrow site on the western flank represents a sediment sink (thus promoting rapid recovery and infilling with like material); 3. The combination of size and position of sand source site results in least impacts to shoal integrity; 4. Dredging to occur during winter months (reduced biological activity); 5. The project will allow for undredged areas in close proximity to be left undisturbed to promote more rapid recolonization of benthos (as was documented for Jay Bird Shoals and Bald Head Creek Shoals with similar post -project conditions); 6. The project will avoid hard -bottom habitat; 7. The project will avoid Primary Nursery Area (PNA) impacts; 8. The project will avoid inlet and associated shoals for large-scale sand volume needs'; 9. The project will utilize hydraulic cutter suction dredge (thereby avoiding and minimizing physical entrainment of species in close proximity to the dredge operation); and 10. The project will include post -project physical monitoring of borrow site (i.e. assessment of physical recovery). The proposed action is not anticipated to have any long-term effects on fishery species. This is due in part to the following considerations: (1) the limited spatial and temporal effects of elevated turbidity due to high sand content of dredged sediments and rapid dilution; (2) the mobility of finfish and associated avoidance behavior; (3) the physical conditions of the dredge site favoring rapid infilling and benthic recovery; (4) avoidance of peak benthic and larval fish recruitment periods during dredging and nourishment; (5) fecundity and opportunistic nature of benthic communities to accommodate anthropogenic and natural disturbance; and (6) the avoidance and minimization measures described above. Given the size of the proposed borrow area relative to the FPS feature (less than 0.5 % spatially and 0.1% volumetrically) and the annual rates of sediment input, the morphological integrity of the t All coastal inlets are designated HAPC for paneaid shrimp, blue crabs, and estuarine -dependent snapper -grouper species. www.lmgroup.net • Phone: 910.452.0001 • Fax: 910.452.0060 3805 Wrightsville Ave., Suite 15, Wilmington, NC 28403 Page 16 shoal will not be affected by the proposed action. Provided the overall physical integrity of the shoals is maintained, then potential adverse effects to ecological functions are minimized. In general, it is preferable to utilize sites that are anticipated to have a high likelihood of physical recovery and biological recovery. The location of the borrow site on the western flank of FPS ensures infilling with sand (consistent with the existing substrate) and a relatively high rate of recharge. In light of the favorable physical conditions of the borrow site (suitable substrate and characteristics favorable for physical and biological recovery), avoidance of other sensitive EFH habitats, adherence to the identified SAFMC protection measures, and incorporation of additional mitigative actions, it is believed that potential adverse ecological effects are minimized. Comment #6: There are numerous questions remaining that need to be addressed before this project should go forward. Staff from BOEM are currently planning to hold a workshop this fall to discuss the state of the science of Frying Pan Shoals and how to move forward in addressing data gaps. Until then, the applicant has a viable alternative, use of Jay Bird Shoals. The NCDMF therefore objects to this permit modification request. Should the project be permitted, the NCDMF requests that the applicant be required to monitor sediment deposition rates and composition, as well as monitor benthic invertebrate composition and change to productivity. The project should be considered a one-time event until all necessary research recommended by NCDMF and the 2020 BOEM workshop is completed and reviewed. Response: The Applicant's consultant (LMG) will be attending the BOEM workshop this Fall. Contemplation of any sand source sites in federal waters (as BOEM is evaluating) would require the use of a hopper dredge and work during environmental moratoriums. As a result, potential ecological effects of such would be significantly greater. With respect to the use of Jay Bird Shoals (JBS), as referenced above, due to both the recent Village - sponsored dredging of JBS and the recent authorization issued to the Town of Oak Island (Action ID Number SAW-2018-02230) to dredge 1.1 Mcy of sand from JBS this coming year (2021), the use of JBS for additional sand nourishment needs is not possible at this time or in the near future. That being said, the Applicant will seek to preferentially utilize JBS should the sand source site demonstrate sufficient physical recovery and sufficient volumes of beach -compatible sand prior to the need for the next locally -sponsored nourishment of South Beach. Note also that this Major Modification request is for a one-time dredge event with both physical and benthic monitoring proposed to evaluate the effects of dredging on FPS prior to any requests for dredging in the future. The Applicant acknowledges the need for the monitoring of physiographic, sedimentary and benthic recovery within the proposed area of excavation. VHBI's engineer (Olsen Associates) believes that based upon the existing precepts of the Wilmington Harbor Sand Management Plan, which episodically places high quality maintenance sand on BHI, it could be necessary to construct an interim locally sponsored beach fill project on 8- to 12-year intervals (more or less). However, the use of JBS for future events could very well provide a viable alternate sand source in lieu of the FPS borrow area. www.lmgroup.net • Phone: 910.452.0001 • Fax: 910.452.0060 3805 Wrightsville Ave., Suite 15, Wilmington, NC 28403 Page 17 II. NC Wildlife Resources Commission Comment and Response Comment #1: Request modeling of sediment transport for determining recovery/recharge. Response: Refer to response to NC DMF Comment #3 above. There have been a number of investigations studying sediment transport along the North Carolina shoreline. The published rates for the two Bald Head Island shorelines which join to form the Cape Fear Point are as follows: • South Beach — 339,300 cubic meters annually toward the East. • East Beach — 341,000 cubic meters annually southward. This represents a potential net annual hypothetical rate of deposition to the Cape Fear Shoal formation of 680,300 cubic meters (i.e. 813,215 cy). Annual monitoring of South Beach by the VBHI indicates that net easterly transport would typically be less than that estimated above. Comment #2: Concern regarding cumulative effects of multi -dredge event project. Response: The Applicant is requesting a one-time dredge event under this Major Modification request for a borrow site area that has been substantially reduced from the prior 2016 request. The Applicant and project engineer have worked to reduce the limits of spatial impacts of the proposed borrow site based upon comments received subsequent to the submittal of the 2016 proposal. Of particular note with respect to avoidance and minimization efforts since the 2016 submittal is the following: the deletion of the dredge access corridor (aka "fairway'); the reduction in borrow site acreage (from 460.1 acres to 198.4 acres); and the limitation of dredging to an initial single borrow event to be monitored. Post -dredge monitoring of physiographic, sedimentary and benthic parameters will be performed to accurately assess the recovery of the borrow site. These data will be evaluated and used for any potential consideration of future dredge events. Note that Olsen Associates believes that based upon the existing precepts of the Wilmington Harbor Sand Management Plan, which episodically places high quality maintenance sand on BHI, it could be necessary to construct an interim locally sponsored beach fill project every 8 to 12 years (more or less). However, the use of Jay Bird Shoals (JBS) for future events could very well provide a viable alternate sand source in lieu of the FPS borrow area. As a result, the potential for any long-term cumulative effects is significantly reduced or avoided. Comment #3: Adherence to applicable environmental windows. Response: The proposed modification requests to perform the work during the acceptable environmental windows and will avoid shorebird and sea turtle nesting periods (combined April 1 to November 15 moratorium). If there is any proposed deviation to the planned dredge and nourishment work window, the Applicant will coordinate with state and federal permitting and resource agencies for appropriate authorization. www.lmgroup.net • Phone: 910.452.0001 • Fax: 910.452.0060 3805 Wrightsville Ave., Suite 15, Wilmington, NC 28403 Page 18 Comment #4: Survey and monitoring reports. Response: The Applicant has performed post -construction monitoring of the terminal groin project with reports submitted on an annual basis to the Corps of Engineers. Comment #5: Concern over repeated beach nourishment projects (higher frequency intervals). Response: Noted. Prior macro -invertebrate monitoring of the beachfront both pre- and post - nourishment (conducted along South Beach and West Beach from 2009 to 2012) revealed that macroinvertebrate taxa fluctuate seasonally. For coquina clams, no statistically significant differences were found between pre -construction and post -construction conditions. For mole crabs and ghost crab burrow hole densities, some significant differences between pre- and post - construction sampling events were identified. However, the statistical (ANOVA) analysis revealed that these fluctuations were likely due to seasonality and other factors not measured in the study rather than project -related activities (since similar differences were observed within control sites). Numerous studies have demonstrated rapid recovery of invertebrate taxa along nourished shorelines (less than one year) provided that the fill material is beach quality sand and similar in texture and composition to the recipient beach (Hackney et al. 1996, Nelson 1993, USACE 2001). Comment #6: Concern regarding beach profile slope (i.e. need to avoid backslope or trough in profile that could trap or disorient nesting sea turtles or hatchings). Response: Noted. The design avoids backsloping of beach profiles. Construction management will include monitoring of the profile to ensure that backslopes or troughs do not occur. Comment #7: Dune revegetation and stabilization should follow resource agency guidelines. Response: Noted. The Applicant will consult with appropriate agencies to implement appropriate methods for dune revegetation and stabilization. Every attempt will be made to complete the dune stabilization measures during the applicable environmental windows. Comment #8: Recommend overview of beach management activities occurring on the Island and the preparation of a single comprehensive management plan. Response: Noted. The project EIS discussed all recent and proposed dredge and beach nourishment projects (for the reasonably foreseeable future). Beach nourishment actions implemented by the Village are also a matter of permit record. A copy of the engineered beach plan outlining beach management activities for the Island is also provided for reference (Attachment B). www.lmgroup.net • Phone: 910.452.0001 • Fax: 910.452.0060 3805 Wrightsville Ave., Suite 15, Wilmington, NC 28403 Page 19 III. NC Division of Water Resources Comment and Response Comment: Please provide more details that addresses the concerns from the NCDMF and the NCWRC regarding practical alternatives and avoidance and minimization of impacts for this project. (15A NCAC 02H .0506(f) and (g)] If these issues are not resolved, the NCDWR will have to move to deny your application as required by 15A NCAC 2H .0506. If these concerns are addressed to the satisfaction of the NCDMF and the NCWRC, the NCDWR will have no objection. Response: Noted. The Applicant is providing responses and additional information to the commenting agencies (namely NC DMF and NC WRC). There have been a number of additional avoidance and minimization measures identified (to be implemented) since the prior 2017 permit modification request. Principally among these measures have been the reduction of the extent of the dredge footprint and confining this modification request to a one-time dredge event to be monitored for the assessment of physical and biological recovery (as described in more detail above). In addition, the Applicant agrees to prioritize the use of Jay Bird Shoals should adequate recovery of that sand source be demonstrated prior to the need for the next Village -sponsored nourishment. Lastly, the project is to employ the protection measures identified by the South Atlantic Fisheries Management Council (SAFMC) specific for dredge and fill projects in areas designated as Habitat Areas of Particular Concern (HAPC) as well as several other measures identified in the responses provided above. As a result, it is the position of the Applicant that the proposed project will not result in a significant impact to EFH (as has been demonstrated for other dredging projects routinely occurring within EFH and HAPC of North Carolina state waters) and therefore does not represent a degradation of state waters. IV. State Historic Preservation Office (SHPO) Comment and Response Comment: The Bald Head Island south beach renourishment project has the potential to affect culturally significant shipwrecks, if avoidance protocols are not enacted. Avoidance is essential given the potential of irreparable damage to cultural resources, as well as to the dredging equipment, as site CF1001 - the Ella is a substantial steel structure. We are aware however that work has been carried out in the area in the past, with the dredging of the channel and the installation of stone jetties (sic). We, therefore, concur with the recommendation outlined in the submitted report from 2016, which states "In the event that the buffered anomalies can be avoided, no additional investigation is recommended in conjunction with the proposed project." To that effect, we offer this "unanticipated discoveries" condition: If additional cultural resource(s) are identified during monitoring and/or construction, all work will be halted within the limits of the resource(s) and the Office of State Archaeology (OSA) will be contacted. Work should move to another area and the Underwater Archaeology Branch should be contacted immediately (910-250-7320). A staff member will be sent to assess the wreckage and determine the proper course of action. The OSA will initiate the coordination required for a determination of eligibility or recovery effort. If after consultation between the County and OSA, additional mitigation is determined necessary, the County, in consultation with OSA, will develop and implement appropriate protection/mitigation www.lmgroup.net • Phone: 910.452.0001 • Fax: 910.452.0060 3805 Wrightsville Ave., Suite 15, Wilmington, NC 28403 Page 110 measures for the resource(s). Inadvertent or accidental discovery of human remains will be handled in accordance with North Carolina General Statutes 65 and 70. Response: Noted. It is understood and agreed that such a condition would be included within the permit authorization for the project. On behalf of the Applicant, we appreciate the opportunity to respond to comments received for the proposed project and your assistance in processing the Major Modification request. Should you have any questions regarding the information provided, please feel free to contact me vial phone at 910-452-0001 or by email at cpreziosi@lmgroup.net. Thank you for your time and assistance. Sincerely, Christian Preziosi Land Management Group (Permit Agent) Encl. Attachment A — Borrow Site Discussion (Olsen Associates) Attachment B — Engineered Beach Plan (Olsen Associates) cc. Jeff Griffin, Village of Bald Head Island Chris McCall, Village of Bald Head Island Erik Olsen, Olsen Associates Tara MacPherson, DCM-Wilmington Ronnie Smith, USACE Wilmington District — Regulatory Branch Sources: Boehlert, G. W. and B.C. Mundy. 1988. Roles of behavioral and physical factors in larval and juvenile fish recruitment to estuarine nursery areas. Am. Fish. Soc. Sym. 3: pp. 51-67. Hackney, C.T., M. Posey, S. Ross, and A. Norris. 1996. A review and synthesis of data on surf zone fishes and invertebrates in the South Atlantic Bight and the potential impacts from beach renourishment. For Wilmington District, US Army Corps of Engineers, Wilmington, North Carolina. McNinch, J.E., 2009, Literature Review of Cuspate Forelands — Implications of dredging Frying Pan Shoals", Report prepared for Wilmington District, USACOE. Morgan, S.G. and J.R. Anastasia. 2008. Proceedings of the National Academy of Sciences, January 8, 2008. Vol. 105 (1): pp 222-227. www.lmgroup.net • Phone: 910.452.0001 • Fax: 910.452.0060 3805 Wrightsville Ave., Suite 15, Wilmington, NC 28403 Page I11 Nelson, W.G. 1993. Beach restoration in the Southeastern US: environmental effects and biological monitoring. Ocean and Coastal Management. 19: 157-182. U.S. Army Corps of Engineers (USACE). 2001. The New York District's Biological Monitoring Program for the Atlantic Coast of New Jersey, Asbury Park to Manasquan Section Beach Erosion Control Project, Final Report. Waterways Experiment Station, Vicksburg, MS. Van Gaalen, J.F., Tebbens, S.F., and Barton, C.C., 2016. Longshore sediment transport directions and rates from northern Maine to Tampa Bay, Florida: Literature compilation and interpretation. Journal of Coastal Research, 32(6), 1277-1301. Coconut Creek (Florida), ISSN 0749-0208. www.lmgroup.net • Phone: 910.452.0001 • Fax: 910.452.0060 3805 Wrightsville Ave., Suite 15, Wilmington, NC 28403 ATTACHMENT A. FRYING PAN SHOALS — BORROW SITE DISCUSSION BACKGROUND The Cape Fear Shoals (FPS) formation has been evaluated as a potential sand source for purposes of beach restoration beginning in the 1970's (Meisburger, 1977). That Reconnaissance level work was carried out by the Coastal Engineering Research Center (CERC) for the Wilmington District, USACOE. Both cores and sub -bottom survey comprised the majority of the data acquisition performed for purposes of defining the spatial distribution of potential sand sources located within FPS. At the time, isopachs of potential sand thickness indicated at least 1.4 billion cubic yards of potential beach quality sand located within the Cape Fear Shoals formation. This estimate is assumed to be conservative. McNinch (2009) performed a Literature Review of Cuspate Forelands which included a discussion of the implications of dredging Frying Pan Shoals. With respect to the latter, Dr. McNinch made the following observations which are relevant to the siting of the proposed VBHI borrow site; * "The most active region of sediment recharge to FPS is likely near the cape point, particularly along the crest of the shoal where it extends seaward from the subaerial cape point and the shore parallel sand bar that merges into FPS from the updrift beach". Note — the updrift beach or shoreline northward of the cape point is known as East Beach on BHI. + Sediment along the flanks of FPS likely migrate crestward during swell conditions and seaward when it reaches the crest". "The crest of the shoal is likely planed -off during storm conditions, when waves are steep and breaking occurs across the shoal, and sediment is transported to the flanks". July, 2020 1 QIsen associates, inn. * "Sediment dredged from the northwest flank of FPS will likely recharge episodically from sediment transported from the crest during storms, particularly extratropical nor' easters". Numerous individuals or organizations have performed estimates of littoral transport along the every -varying shoreline components of the State of N.C. More recently, (Van Gaalen, Tebbens and Barton, 2016) have summarized sediment transport directions from Northern Maine to Tampa Bay, FL. For the Cape Fear formation, the published rates for the two BHI shorelines which join to form the Cape Fear Point (see Figure 1) are as follows- * South Beach — 339,300 cubic meters annually toward the East, • East Beach — 341,000 cubic meters annually southward. This represents a potential net annual hypothetical rate of deposition to the Cape hear Shoal formation of 690,300 cubic meters (i.e. 813,215 cy). Note — annual monitoring of S. Beach indicates that net easterly transport would typically be less than that estimated above, In 2009, the Wilmington District, USAGE acquired some 31 Vibracores in proximity to the western side of Frying Pan Shoals as part of a sand search for the Brunswick County Shore Protection Project, The District then contracted with Catlin Engineers and Scientists of Wilmington, N,C, to analyze the cores. A summary of findings was provided to the Wilmington District on 27 May 2010 (Catlin, 2010). The report included core logs, grain size classifications and various summaries of the sediment characteristics encountered suitable for beach restoration. In 2016, Olsen Associates, Inc, initiated a multi -phase Sand Search Investigation of Frying Pan Shoals (Olsen, 2016) intended to allow for the permitting, of a borrow site within State waters. July, 2020 2 olsen associates, inc. The chronological Task Logic for the phased Sand Search sponsored by the VBHI can be summarized as follows: I . A coarse grid survey was performed to update general bathymetric shoal features within the 3-mile limit. Mapping utilizing federal NOS data was not reliable for purposes of coring. 2. A Phase I (coarse grid) Cultural Resource Investigations was carried out to eliminate any dense clusters of magnetic anomalies which would indicate a high probability of a ship wreck site. It was determined that no level of geotechnical investigation would be performed in any such areas identified. 3. Based upon 1.) and 2.) above, a Vibracoring Plan was formulated so as to maximize potential depths of beach compatible sediment, with the intent of minimizing future conflicts with probable cultural resource locations. 4. Subsequent to coring, a sub -bottom survey was performed to extend the data base between cores and to areas of interest where cores would not be feasibly (or safely) acquired due to shallow depths, breaking waves, or tidal surging, S. In consideration of the results of the seismic survey, Vibracore logging and laboratory analyses of sediment samples over depth, a generalized borrow area was defined by Olsen Associates, Inc. — all of which is documented in a comprehensive report (Olsen, 2016). 6. Subsequently, a Phase II Cultural Resource Investigation was performed of the selected borrow area in order to eliminate areas of avoidance recommended by the project marine archaeologist. The final Permit Application was based upon the refined borrow site limits which included buffers between, or around unverified anomalies and future dredging activities. July, 2020 1 Qlsen associates, inc, BORROW SITE SELECTION The selection of the proposed 188.7 A. area borrow site was determined on the basis of both environmental and physical characteristics, Although the engineering design of the proposed borrow site is a matter of record (Olsen, 2016), in order to minimize environmental impacts, the following relevant selection parameters were prioritized: Borrow Site Recovery — As recommended by McNinch (2009), the proposed area of excavation is principally located on the crest of the existing shoal formations which is the most high energy (i.e. dynamic) portion of the shoal. This will assure rapid post - construction deposition of new material into the excavated area. AIthough it is not possible to reliably "numerically model" the infilling process due to the complexity of the shoals ever changing bathymetry, it can be reliably estimated based upon the anticipated volume of material which episodically enters the shoal formation from the two (2) shorelines on BH1 which form the Cape Point. A conservative engineering estimate of the ability of the FPS borrow area to recover 80-90% of the neat volume removed is 10 years, or less. • Borrow Site Substrate — For purposes of rapid benthic recovery, the post -excavation substrate should be self -similar to existing prior to dredging. This is addressed two ways: a) by ensuring that the depth of excavation is strategically limited such that the sediment exposed (post -dredging) has similar granular characteristics to the native seabed, and b.) by ensuring that material transport into the excavated area will be rapid and continuous. Under such constraints, benthic recovery of the "disturbed" seabed typically occurs within I -year. • Minimization of the Area Impacted — For purposes of reducing temporal dredging impacts to pre-existing benthic resources, it is desirable to design a borrow area having the smallest effective "foot print". For this site, this is accomplished principally through the utilization of a cutter suction dredge, as well as the specification of a dredged area with the thickest layer of sediment available — which for the FPS formation is synonymous with the centralized portion of the shoal. Although the depth of excavation July, 2020 4 Olsen associates, Inc. at that location may exceed 15 ft. below the seabed, it is reliably predicted that shoal dynamics at this location will quickly reduce the effective borrow depth due to rapid infilling and slope adjustments. Note — A secondary benefit of a cutter suction dredge is that it does not "entrain" fishery resources — in contrast to a hopper dredge which represents a quantifiable threat to fishery resources during the dredging process including endangered species such as the Atlantic Sturgeon. * Frequency of Occurrence — The Applicant's consultant has opined that based upon the existing precepts of the Wilmington Harbor Sand Management Plan, which episodically place high quality maintenance sand on BHI, it could be necessary to construct an interim locally sponsored beach fill project every 8-12 years, mot. It is acknowledged however, that subsequent to the first use of the FPS borrow site, it could be possible that the Agency preferred borrow area located at Jay Bird Shoals may have sufficiently recovered by that time. As such, it could provide a viable alternate sand source in lieu of the FPS borrow area. • Confirmation of Impact and recovery Predictions — The VBHI as Applicant for the development of the FPS borrow site acknowledges the need for the monitoring of physiographic, sedimentary and benthic recovery within the proposed area of excavation. July, 2020 5 Qlsen associates, inc. REFERENCES Catlin, Engineers and Scientists, 2010, Brunswick County Beaches Renourishment Study — Frying Fan Shoals Soil Testing and Compatibility Analysis and Geotechnical Report", report prepared for Wilmington District, USACOE, Catlin Wilmington, N.C. 28404. McNinch, J.E., 2009, Literature Review of Cuspate Forelands — Implications of dredging Frying Pan Shoals", Report prepared for Wilmington District, USACOE. Meisburger, E.P., 1977. "Sand Resources on the Inner Continental Shelf of the Cape Fear Region, N.C.," U.S. Army Corps of Engineers, CERC, Ft. Belvoir, VA, Misc. Report No. 77-1. Olsen Associates, Inc., 2016. "Frying Fan Shoals — Sand Search Investigation", report prepared for Village of Bald Head Island. Olsen Associates, Inc., 2618 Herschel St., Jacksonville, FL 32204. Van Gaalen, J.F.,: Tebbens, S.F., and Barton, C.C., 2016, Longshore sediment transport directions and rates from northern Maine to Tampa Bay, Florida: Literature compilation and. interpretation. Journal of Coastal Research, 32(6), 1277-1301. Coconut Creek (Florida), ISSN 0749-0208. July, 2020 6 Q18en associates, inc. pie 0 11 0 Prepared for: Village of Bald Head Island Prepared by: Olsen Associates, Inc. 2618 Herschel Street Jacksonville, FL 32204 (904) 387-6114 (Fax) 384-7368 olsen-associates.com C-1468 nk �— --- — —1 Sept. 2018 olsen associates, inc. PREFACE In February 2009, Olsen Associates, Inc. issued a documentation report entitled "Village of Bald Head Island, Engineered Beach Project". The following report (dated September 2018) serves to update the earlier report in anticipation of the predicted impacts associated with Hurricane Florence to the North Carolina coastline and more specifically to Bald Head Island. It is noted that during the period 25 August to 1 September 2011, Hurricane Irene caused impact to Bald Head Island's "engineered beach" project. In accordance with FEMA Declaration No. 4019 DR NC, Project Worksheet (PW) BHGJS03 allowed for Category `G' sand placement along a portion of South Beach impacted by the event. Subsequently PW No. BHGJS0300588 was issued for the replacement of five (5) damaged sand tube groins. Sept. 2018 - i - olsen associates, inc. DOCUMENTATION FOR THE VILLAGE OF BALD HEAD ISLAND, NC ENGINEERED BEACH PROJECT PURPOSE In 1998, the Village of Bald Head Island formally embarked on a long-term Plan for Island -wide Beach Management. Simplistically, the goal was to develop an "engineered" solution to beach erosion along South Beach and portions of West Beach, both of which are physically interrelated through a common littoral sand sharing system. At the present time the program of improvement is based upon three (3) major components: a) Large scale beach restoration through sand placement volumes sufficient to create and maintain natural beach widths and dimensions capable of protecting publicly funded upland infrastructure, habitable structures, etc. b) The reconstruction and maintenance of a complimentary sand tube groin field at the west end of South Beach intended to reduce (but not eliminate) sediment losses from the beach fill to the adjacent federal navigation project channel which serves the Port of Wilmington, NC., and c) The introduction of a 1,300 ft. terminal groin constructed in 2015 at the juncture of South Beach and the Cape Fear River. The design intent of the low profile rock structure is to create an updrift sand fillet sufficiently broad enough so as to maintain an improved shoreline orientation and berm width in an area of chronic erosion — where beach fill alone has been incapable of reliably protecting upland properties and infrastructure. Two sources of beach quality sediment were preliminarily identified for purposes of project construction and maintenance. The principal sand source was determined to be clean littoral material routinely derived from improvements to, or ongoing maintenance of, a portion of the entrance channel to the federally sponsored Wilmington Harbor Navigation Project. The second primary source of available material was borrow site(s) developed from abutting shoal formations which had been deposited as a direct result of the navigation project. Utilization of Sept. 2018 - 1 - olsen associates, inc. VBHI — Engineered Beach Project the latter sand source was determined to be a practical means of re-establishing natural sand bypassing at the mouth of the Cape Fear River which had been eliminated by the navigation works constructed at that location in the 1800's. Currently, the Village is likewise investigating the development of a longterm borrow site within the extensive Cape Fear Shoals formation lying seaward of the eastern end of Bald Head Island. BACKGROUND Since about 1974, beach erosion experienced along portions of the Bald Head Island shoreline, NC has been principally manifest as "chronic" — with severe shoreline recession along South Beach (most particularly the western portion nearest the inlet) and the seawardmost segment of West Beach. The island's historical erosion is the apparent result of several combined factors: (1) divergent alongshore littoral transport gradients near the center of South Beach, (2) tidal currents and proximity to the Cape Fear River Entrance, (3) direct recurring impacts associated with high frequency dredging operations required by the adjacent deep draft federal navigation project, and (4) long term morphological changes in island configuration and offshore ebb tidal shoal formations due to initial navigation channel construction, long term maintenance practices and more recently, entrance channel deepening, widening and realignment in 2000. The Wilmington Harbor Entrance Channel, which extends several miles seaward of Bald Head Island, is not stabilized by jetties and until a channel reconfiguration in 2000, had been maintained at a single location and orientation by dredging since the late 1800's. In recent times, but prior to the 2000 major modifications, maintenance of the entrance channel typically required the removal and offshore disposal of between 500,000 — 1,000,000 cubic yards (cy) of beach quality material each year. Beginning in 2000, the portion of the federal navigation channel abutting Bald Head Island was deepened by four feet, widened at several locations, and reoriented (see Figure 1). It is important to understand that the seven mile long offshore ocean entrance segment of the navigation project was reoriented as part of the deepening project from its historical location to a new location directly seaward of Bald Head Island through Bald Head Shoal. The documentation of recurring impacts due to deepening, widening and reorienting the channel in the vicinity of Bald Head Island has been a major focus of a Village sponsored annual Sept. 2018 - 2 - olsen associates, inc. t .p'. if �n� � rs Hu¢- • I... 1 F f � � f � )~ �.LA�,A.. 1 � r � �� r` I r' \ yiyl y' 1 '�� ' � rr •� 1 � €�J� _. 4/ _ � a I� - �-.� ` -i. F i. ��r�-•g!'� k0 �*0 i' � _"''r 3 '-1� f — Oh Is 1 ! .J4 -� 1 &^ P - •� �,4 'NI z}I- > ' ,;r 2��s.Y fAS ri!'I d4 � "',f �� CJ """rrr 111 e till 17 -24 15 12 P4 ��yy ' I �L A N' d Pa f1 is .33 .. J :I� „?� � . yam` � �. � P'.••'i -. '- -33 • . r` -39 A. r ' t In 750 0 I500 '1F700 �,�' 59000FT 2006 CONTOUR DATUM: NGVD 29 NAUTICAL CHART DATUM: MLLW 2006 SURVEY-GEODYNAMICS, INC FIGURE 1 LOCATION OF BALD HEAD ISLAND RELATIVE TO FEDERAL NAVIGATION PROJECT -3- VBHI — Engineered Beach Project beach monitoring program. The latter was initiated in 1999 prior to, as well as in response to, the ocean entrance channel's proposed reconfiguration and widening by the federal government. As of May 2018, sixteen comprehensive Annual Monitoring Reports have been published (see REFERENCE SECTION). PLAN OF ACTION In order to facilitate a long-term program of engineered beach restoration, the Village of Bald Head Island adopted a shore stabilization strategy predicated upon navigation project related mitigation by State and Federal interests as the primary source of funding for sand placement. Secondary sources of funding, as necessary, have derived from Village annual revenues, the State of North Carolina and more recently the establishment of on -island special purpose Taxing Districts. The latter are directed toward beach management and enhancement activities and, in particular, beach restoration and ancillary shore stabilization structures constructed and maintained by the Village as part of a longterm Plan. For purposes of facilitating a major harbor deepening and widening program in 2000, the Wilmington District USACOE formulated a project specific action element entitled the Wilmington Harbor Sand Management Plan (WHSMP). The Plan was codified by State permit for purposes of meeting State of North Carolina Coastal Zone Consistency requirements. For the most part, the Plan was in direct response to the stated concerns and associated legal action(s) by the Village of Bald Head Island (VBHI) regarding both historical channel maintenance impacts and potential new impacts of the deepening project to both the regional sediment budget and Bald Head Island. The Plan's purpose was to reverse the highly impactive "standard practice" of transporting beach quality sand removed from the channel during dredging activities to deep water offshore disposal sites. Specifically the Plan called for the future placement of all dredged beach quality sand directly onto adjacent beaches with special emphasis on Bald Head Island. The initial construction of the widening/deepening project provided over 5 Mcy of high quality sediment in 2000. Approximately 1.85 Mcy of that volume was used to initially improve the entirety of South Beach at Bald Head Island. Over a typical six -year maintenance cycle, the Wilmington Harbor Sand Management Plan proposed that approximately 1.0+ Mcy of sand predicted to be dredged biannually as maintenance would be placed on the Beaches of Bald Head Sept. 2018 - 4 - olsen associates, inc. VBHI — Engineered Beach Project Island in year two and four (after initial construction) and on Oak Island/Caswell Beach during year six. The 6-year cycle would then repeat. The two-year dredge and disposal cycle was planned for the life of the project but is subject to alteration based upon impact documentation and other relevant factors. Pragmatically, implementation can likewise be affected by Congressional funding of such navigation works, etc. To date, federal funding shortfalls associated with direct sand placement have been addressed by both the State of North Carolina and the Village of Bald Head Island. At this time, it is relatively clear that the Wilmington Harbor Sand Management Plan provides a partial framework for the implementation of an "engineered" beach at Bald Head Island. Since initial construction of the deepening project in 2000, six maintenance dredging operations have been conducted within three inner channel segments closest to Bald Head Island. Monitoring has conclusively shown that Bald Head Island needs sand every two to three years, not the SMP's two out of three biennial events, Even though the placement of sand is procedurally viewed as "disposal" by the USACOE, the tenets of the federal Plan allow the coastal engineering consultant to the Village of Bald Head Island to strategically define the limits of work and design templates to be filled throughout the project disposal area. By virtue of a project specific updated "design", based upon comprehensive annual beach monitoring, the Village of Bald Head Island is able to implement an engineered beach restoration project. As an adjunct to the beach restoration project, the Village maintains a multi -structure sand tube groinfield intended to limit shoreline recession in the area of most severe erosion nearest the inlet channel. The groin field was required by, and is viewed as a favorable project element by the USACOE since it correspondingly tends to reduce the amount of sand entrainment caused by the navigation channel — and particularly immediately after each beach fill placement operation at South Beach. In 2015, this groinfield was supplemented by the construction of a 1,300 ft. long rock terminal groin — intended to further increase the longevity of future beach fills constructed eastward thereof on South Beach. HISTORICAL EROSION CONTROL ACTIVITIES Beach Construction. Major beach construction activities constructed at Bald Head Island since 1991 are summarized in Table 1. The three small scale privately initiated channel disposal Sept. 2018 - 5 - olsen associates, inc. VBHI — Engineered Beach Project projects constructed between 1991 and 1997 were cost -shared or paid for in their entirety by the Village of Bald Head Island. Limited in scope, the three early sand placement efforts were not highly successful in providing meaningful levels of shore stabilization due to their size. As a result, the Village of Bald Head Island eventually adopted the long-range plan -of -action discussed herein, i.e., comprehensive beach restoration via an "engineered project" construction and commitment to long-term maintenance. That Plan -of -Action addressed both South Beach and West Beach. Table 1: Beach construction activities at Bald Head Island since 1991. Year Volume Sponsor Location 1991 0.35 ± Mcy VBHI (Sta. 24+00 to 138+00) 1996 0.65 ± Mcy VBHI (Sta. 24+00 to 142+00) 1997 0.45 ± Mcy VBHI (Sta. 24+00 to 128+00) 2001 1.849 ± Mcy USACE* South Beach (Sta. 41+60 to 205+50) 2005 1.217 ± Mcy USACE* South Beach (Sta. 46+00 to 126+00) 2006 47,800 cy VBHI West Beach (Sta. 16+00 to 34+00) 2007 1.1± Mcy USACE* South Beach (Sta. 46+00 to 174+00) 2009/10 1.850 :L Mcy VBHI West Beach (Sta. 8+00 to 32+00) South Beach (Sta. 40+00 to 190+00) 2012 137,990 cy FEMA/VBHI West Beach & Western South Beach 2013 1.566 ± Mcy USACE* South Beach (Sta. 44+00 to 150+00) 92,500 cy West Beach (Sta. 8+00 to 27+00) 2015 1.33 ± Mcy USACE* South Beach (Sta. 41+50 to 154+00) 2016/17 50,000 cy VBHI West Beach and Row Boat Row * Disposal pursuant to the WHSMP The initial 2001, 1.849 Mcy comprehensive beach restoration project was constructed as an element of the Wilmington Harbor Deepening Project. The disposal sand was placed in the configuration of a designed berm along the entirety of the 15,500 feet of shoreline at South Beach. The limits of work and design templates were provided to the Wilmington District by Olsen Associates, Inc. on behalf of the Village. All work was performed in conformance with the requirements of the SMP. The 2005, 1.2 Mcy beach disposal project was the initial "maintenance" event (Year 2 of the SMP) of the scheduled disposal cycle and was constructed Sept. 2018 - 6 - olsen associates, inc. VBHI — Engineered Beach Project between November 2004 and January 2005. The 2006, non -Federal West Beach sand disposal project was independently constructed by the Village in January 2006. Sand for that work was sourced from Bald Head Creek. The 2007, 1.1 Mcy disposal project was the second declared "maintenance" event (Year 4 of the SMP) and was constructed between February and April 2007. Approximately 1,098,000 cubic yards (pay volume) of beach quality material was placed along the South Beach shoreline in accordance with a fill design requested by the Village. In 2009/10, the terms of the WHSMP dictated that the scheduled channel maintenance sand be placed on Oak Island, in lieu of Bald Head Island. As a result, the Village constructed a 1.85 M cy beach fill along the majority of South Beach and a small section of West Beach which fronts the inlet throat. The sand source was a borrow site developed and permitted by the Village in Jay Bird Shoals. Portions of that borrow site continue to be available as a sand source today. Detailed documentation for this Village project is included in Olsen (2010). It is noted that the entire 16 sand filled tube groinfield was replaced immediately subject to beach fill completion. Subsequent to the passage of H. Irene in 2012, a FEMA funded small scale fill project was constructed along the western end of S. Beach. Five (5) sand tube groins damaged by the storm were also replaced as part of that project. The project sand source was Bald Head Creek. In 2013, the Wilmington District placed approximately 1.6 Mcy of channel maintenance material along S. Beach and 92,500 cy along the southerly section of West Beach. Similarly in 2015, the District placed approximately 1.33 Mcy on South Beach with material sourced from routine channel maintenance of the Cape Fear Entrance Channel (inner 3 sections). Erosion Control Structures (1996 to 2018) — Synopsis Erosion control structures constructed at Bald Head Island since 1996 are summarized in Table 2. A detailed discussion of the history of erosion control structures is provided in Monitoring Report No. 15 (Olsen 2017). Sept. 2018 - 7 - olsen associates, inc. VBHI — Engineered Beach Project Table 2: Chronology of shore stabilization structures at Bald Head Island since 1994. Year Location Description 1994 Western South Beach Sand bag revetment located along 645 feet of the back - beach berm 1996 Western South Beach Sixteen (16) soft groins (geotube-type structures) were March constructed of geotextile material and sand fill Rehabilitation of 1994 constructed sand bag revetment. 2003/2004 Western South Beach Revetment lengthened by approximately 200 feet and base width increased to 40 ft and crest elevation raised to +12 ft-NGVD . Replacement of 1996 constructed sand tube groin field. 2005 Minor changes in groin location were made in an effort to (January to Western South Beach improve performance. Similarly, experimental "tapered" March) tubes were deployed in an attempt to better accommodate beach rofile recession over time. Complete rehabilitation of the sand tube groin field. 2009 Western South Beach Some adjustment of groin lengths, and the westward relocation of groin no. 16 were made in an attempt to refine the project design. 300 ft sand bag revetment was constructed on the 2011 Western South Beach downdrift (western side) of the last sand tube groin in order to protect several endangered residential structures. In the spring of 2013, the westernmost five (5) sand tube groins were replaced in their entirety. This work was co- 2013 Western South Beach funded by FEMA as part of a post -Irene damage mitigation effort. The project P.W. was BHGJS04 in accordance with FEMA declaration 4019 DR NC. In the spring of 2015, construction was initiated on a single 1,300 ft. long rock terminal groin designed to complement future placement of beach fill at South 2015 Western South Beach Beach. At that time, the westernmost three (3) geotube groins were removed in their entirety. A detailed description of the project is provided in Monitoring Report No. 15 Olsen 2017). The two marina entrance channel structures seaward of 2015 Bald Head Marina Row -Boat -Row originally constructed by Bald Head (West Beach) Island, Ltd., were modified through the addition of rock extensions. Row Boat Row Two (2) detached breakwaters were constructed just 2017 (West Beach) north of the Marina Entrance. Construction details are provided in Section 1.5.3 of this report. Note — As of Sept. 2018, all sand tube revetments are buried within a protective dune system. Sept. 2018 - 8 - olsen associates, inc. VBHI — Engineered Beach Project The structures which effectively contribute to the stabilization of Bald Head Island's engineered beaches — as of the date of this report — are as follows: • S. Beach — 0 1,300 ft. long terminal groin constructed in 2015; o A sand filled tube groin field (originally 16 strux; 3 removed in 2015). • W. Beach o Rubble mound rock jetties at the marina entrance channel constructed in 2015. o Two rock breakwaters constructed in 2017 seaward of Row -Boat -Row. PROJECT DESIGN South Beach. The project renourishment design for South Beach calls for the placement of approximately 1 Mcy of sand every two to three years from the local navigation project with supplementary renourishment, as required, from alternate borrow source(s) developed and permitted by the Village. The project likewise provides for the continued use of structures at the western end of the South Beach fill segment, intended to increase project life. The project limits on South Beach extend approximately from Sta 045+47 to Sta 210+00, or nominally about 16,000 ft. plus fill tapers at both ends (see Figure 2). A typical fill template for S. Beach is depicted by Figure 3. Appendix A to this document includes beach profiles which depict the conditions of the project beaches along South Beach as they existed in May 2018 — prior to the 2018 hurricane season. Normally project fills are constructed within a permit required environmental window which necessitates that completion of fill activities occur between Nov. and April of any one year — except during emergency situations where waivers may be granted. West Beach. The island's "engineered beach" systems likewise includes an approximate 2,100+ ft. long segment of shorefront along West Beach (see Figure 2). Given the steep nearshore slope of the submerged portion of this river -affected shoreline, a fill density of 30 cy/ft. is typically the maximum for this area (see Figure 3). Including tapers, the net fill episodically placed at this location is estimated at about 100,000 cy, or less. West Beach shoreline conditions are likewise comprehensively monitored annually by the Village of Bald Head Island. Sept. 2018 - 9 - olsen associates, inc. o CROCK BREAKWATERS (2) Q 0 m 3 0 m ---ROCK J ETTI ES (2) 2 U W m TERMINAL THE'' GROIN POINTY U3 TR ROAN FjE�O Uxl SCALE 0 700 1400FT _April 2018 Photo September 2018 10 RAi n I-IFAn IcI ANn ( - SECTION OF ENGINEERED BEACH �- N" CAPE FEAR Figure 2: Locations of Engineered Beaches and Stabilizing Structures olsen associates, inc. LIMIT OF PROJECT EASEMENT DISTANCE VARIES — EXISTING DUNE O (VARIES) LIMITOFWOM (w7 �Cti o 71r +8.0' NGVD SOUTH BEACH ATLANTIC OCEAN AVERAGE BEACH FILL DENSITY APPROX. 100cy/ft BEACH FILL MHW (2.5' NGVD) EXISTING BEACH-- SSUMED FILL TEMPLATE SLOPE PROFILE (TYP) '//�%/,\`j/�tj DURING CONSTRUCTION NOTE: 1) FILL DENSITY TO VARY SPATIALLY DEPENDING ON CONDITION OF BEACH AT TIME OF CONSTRUCTION. 2) GROIN FILLET FILL DENSITY VARIES AND MAY EXCEED 300 CY/FT LOCAL TIDAL DATUMS MHHW +2.8 MHW +2.5 NAVD +1.1 NGVD(29) 0.0 MLW -1.8 MLLW -2.0 DUNE 8'NGVD CONDITIONS VARY �\ BEACH FI NOTE: 1) POINT FILL DENSITY MAYBE TYPICAL OF EITHER S. BEACH OR W. BEACH 12TO -15FT NGVD (TYP) LOPEINTERCEPT TYPICAL SECTION OF FILL TOE AVERAGE FILL DENSITYHW (+2.5' NGVD) APPROX. 30-50cy/ft !' (TYP) - 0 LW (-1.8' NGVD) TYPICAL SECTION NTS DATUM: NGVD 29 WEST BEACH m CAPE FEAR RIVER CHANNEL GORGE EXISTING PROFILE (TYP) NTS DATUM: NGVD 29 NOT FOR PURPOSES OF CONSTRUCTION Olsen DATE APPROVED REVISION �}= associates, inc. VILLAGE OF BALD HEAD ISLAND 2618 Herschel Street ENGINEERED BEACH PROJECT FIGURE 3 Jacksonville, FL. 32204 4;• 4) 387-6114 C-1468 TYPICAL BEACH FILL SECTIONS _ • • • C-1 VBHI — Engineered Beach Project In 2016/17, the West Beach segment of improved shorefront was extended to include some 1,400 ft. of shorefront located northward of the marina entrance — typically referred to as Row -Boat - Row (see Figure 2). Stabilizing structures maintained at that location include two (2) rock breakwaters constructed in 2016, and four (4) low profile groins last renovated in 2005. Row - Boat -Row is separated from the southerly portion of West Beach by two (2) rock jetties constructed in 2015. The latter structures protect the marina entrance channel which is an integral part of the island's water -borne transportation system which is served only by ferry and barge. Photographs of stabilizing structures discussed herein are included in Appendix B. PROJECT DOCUMENTATION In order to document shoreline changes along the South Beach and West Beach portion of the island's "engineered" beaches, the Village of Bald Head Island has routinely funded an in- depth annual beach monitoring program. Since 1999, the program has been expanded from annual surveys to include two (2) surveys (spring and fall) and two (2) aerial overflights which result in digital, rectified shoreline photography. An annual report of findings is published which addresses both the prior 12-month period as well as special events (i.e., dredge operations) and other longer term trends are included. The monitoring program specifically addresses beach fill performance and provides guidance for the design of each episodic sand placement operation. The spring hydrographic surveys are scheduled to document beach conditions immediately prior to each hurricane season in order to comply with FEMA related post -disaster eligibility requirements. The beach monitoring program presently being implemented by the Village of Bald Head Island's engineered beaches is based upon a baseline with survey stationing located on approximate 400 ft centers. As shown by Figure 4, the baseline limits extend from Row -Boat - Row, located northward of the entrance to the Bald Head marina (Sta 0+00) southward along West Beach some 4,500 ft to the "Point" (or depositional spit) abutting the existing navigation project channel and thence eastward to Cape Fear along South Beach, an additional 17,300 ft, mol. The baseline stationing is referenced to the North Carolina State Plane Coordinate System, North American Datum of 1927 (NAD27). Sept. 2018 - 12 - olsen associates, inc. RB.1� 18+72 R8.2_ 39+72 O RR-3— r a. -12+00 R8 4— Q RB-5__ O "4.00 jr B-01------� 0+00 8-02 2+pp 4+p0 8-03_ 6+00 8+00 2 8.04 _ ---- 10+00 Q u+0p MW 8-05_ - 14+00 CO B-0p 18+ppLU 20 +00 8-07_ 22+00 24+p0 8.08_ 26+00 28+00 09 3p+471i 3zThe Point" + a, 00 (North of ak °O � Terminal Groin) 3e / ro "The Point" (South of p$o Terminal Groin) 00+05 s ti o� 10 y c01j L' 'r' ".7 ti o R a i• 4 EO-0I iBAr� 1�grg0 SOS ibgrg0 � I m m m m m m m m m m ° m 9 SCALE 0 700 1400FT April 2018 Photo September 2018 13 on CAPE FEAR Figure 4: Island -wide beach monitoring baseline. olsen associates, inc. VBHI — Engineered Beach Project Some level of beach monitoring has been performed at Bald Head Island since about 1990. Initially, surveying was limited to beach profiles from the back berm to a wading depth. In the mid-1990's offshore profiles to a depth of -30 ft or a distance of 3,000 ft were added to the program. In 2009, the program was expanded to include East Beach — pursuant to the request of property owners at that location (see Figure 4). As a result, the entire monitoring baseline length exceeds30,000 ft. Tidal Datums — The elevations and water depths along each of the survey profiles are referenced to National Geodetic Vertical Datum of 1929 (NGVD29). The relationship between NGVD29 and various tidal datums are as follows: Table 3: Tidal datums for Bald Head Island. North Carolinas. Datum Elevation (ft-NGVD 292) Mean Higher High Water (MHHW) +2.82 Mean High Water (MHW) +2.53 NAVD 1988 +1.10 Mean Tide Level (MTL) +0.35 NGVD 1929 0.00 Mean Low Water (MLW) -1.81 Mean Lower Low Water (MLLW) -1.98 ' Approximations based upon extrapolation from Southport, N.C. 2 NGVD 1929: National Geodetic Vertical Datum of 1929 (1929 Mean Seas Level). Horizontal coordinates are referenced to the North Carolina State Plane Coordinate System, North American Datum of 1983. PROJECT PUBLIC ASSISTANCE ELIGIBILITY Section 102(8) of the Stafford Act defines a public facility owned by a State or local government as any flood control, navigation, irrigation, reclamation, public power, sewage treatment and collection, water supply and distribution, watershed development, or airport facility; any non -Federal -aid street, road or highway; any other public building, structure, or system, including those used for educational, recreational, or cultural purposes; and any park. Additionally, Title 44 of the Code of Federal Regulations (CFR), Section 206.201(c) includes an improved and maintained natural feature in the definition of a facility. 44 CFR 206.221(d) defines an improved property to mean a structure, facility or item of equipment that was built, constructed or manufactured. Publicly -owned engineered beaches are eligible for assistance Sept. 2018 - 14 - olsen associates, inc. VBHI — Engineered Beach Project because they are improved natural features, assuming they have been regularly maintained prior to the disaster. The engineered beach segments at Bald Head Island, N.C. meet the criteria of a publicly -owned non -Federal engineered beach. Concurrent with ongoing commitments by the Village to fund the project construction, the local sponsor has the capability and intent to facilitate or perform the requisite future maintenance of the beach fill project for the long-term project life of greater than 30 years. Section 206.226 Restoration of damaged facilities, further defines eligibility criteria for Beaches. For an improved beach, work to re-establish the beach as infrastructure may be eligible under the following conditions: a) The beach was constructed by the placement of sand (of proper grain size) to a designed elevation, width and slope, and b) A periodic maintenance program involving periodic renourishment of sand has been established and adhered to by the Applicant. Implicit in these regulations is the requirement of an Applicant to document the condition of the affected shoreline prior to impact by the storm which results in the declared disaster. As noted above, the comprehensive beach monitoring program implemented annually by the Village of Bald Head Island specifically seeks to fulfill that requirement. POST -STORM ACTION PLAN Immediately subsequent to a major storm event for which a formal disaster declaration may (or will in all probability) be issued, the Village will initiate the following Action -Plan elements: • A comprehensive survey of the affected beaches by a certified hydrographic survey firm, • Concurrent drone photography and eventual digital orthophotography (island -wide), • Analysis of storm induced shoreline volumetric erosion, shoreline recession, vegetation/dune impacts, etc., • Assessment and documentation of damage to infrastructure and development, Sept. 2018 - 15 - olsen associates, inc. VBHI — Engineered Beach Project • The formulation of an engineering report of post -storm conditions suitable for review and consideration by FEMA staff authorized to issue P.W.'s. • The submittal of all relevant documentation as to the existence of an "engineered beach" required by FEMA staff, and • As applicable, any requested letters -of -opinion, computations, or recommendations, by a State of N.C. registered coastal engineer requested by FEMA, Brunswick County or the State of NC. Sept. 2018 - 16 - olsen associates, inc. VBHI — Engineered Beach Project REFERENCES Olsen Associates, Inc. (2003). "Bald Head Island, N.C. Beach Monitoring Program Report No. I (Nov. 1999 — May 2003)", Report prepared for Village of Bald Head Island. Olsen Associates, Inc. 2618 Herschel St., Jacksonville, FL 32204. 66 pp plus app. (June 2003). Olsen Associates, Inc. (2004). "Bald Head Island, N.C. Beach Monitoring Program Report No. 2 (May 2003 — April 2004)", Report prepared for Village of Bald Head Island. Olsen Associates, Inc. 2618 Herschel St., Jacksonville, FL 32204. 51 pp plus app. (August 2004). Olsen Associates, Inc. (2005). "Bald Head Island, N.C. Beach Monitoring Program Report No. 3 (May 2004 — April 2005)", Report prepared for Village of Bald Head Island. Olsen Associates, Inc. 2618 Herschel St., Jacksonville, FL 32204. 38 pp plus app. (December 2005). Olsen Associates, Inc. (2006). "Bald Head Island, N.C. Beach Monitoring Program Report No. 4 (April 2005 — May 2006)", Report prepared for Village of Bald Head Island. Olsen Associates, Inc. 2618 Herschel St., Jacksonville, FL 32204. 40 pp plus app. (July 2006). Olsen Associates, Inc. (2007). "Bald Head Island, N.C. Beach Monitoring Program Report No. 5 (June 2006 — May 2007)", Report prepared for Village of Bald Head Island. Olsen Associates, Inc. 2618 Herschel St., Jacksonville, FL 32204. 37 pp plus app. (December 2007). Olsen Associates, Inc. (2008). "Bald Head Island, N.C. Beach Monitoring Program Report No. 6 (June 2007 — May 2008)", Report prepared for Village of Bald Head Island. Olsen Associates, Inc. 2618 Herschel St., Jacksonville, FL 32204. 40 pp plus app. (August 2008). Olsen Associates, Inc. (2009). "Bald Head Island, N.C. Beach Monitoring Program Report No. 7 (June 2008 — May 2009)", Report prepared for Village of Bald Head Island. Olsen Associates, Inc. 2618 Herschel St., Jacksonville, FL 32204. 49 pp plus app. (August 2009). Olsen Associates, Inc. (2010). "Bald Head Island, N.C. Beach Monitoring Program Report No. 8 (June 2009 — May 2010)", Report prepared for Village of Bald Head Island. Olsen Associates, Inc. 2618 Herschel St., Jacksonville, FL 32204. 64 pp plus app. (August 2010). Olsen Associates, Inc. (2010). "Village of Bald Head Island, N. C. Beach Renourishment Project Post -Construction Report (July 2010)", Report prepared for Village of Bald Head Island. Olsen Associates, Inc. 2618 Herschel St., Jacksonville, FL 32204. 34 pp plus app. (August 2010). Sept. 2018 - 17 - olsen associates, inc. VBHI — Engineered Beach Project Olsen Associates, Inc. (2011). "Bald Head Island, N.C. Beach Monitoring Program Report No. 9 (May 2010 — May 2011)", Report prepared for Village of Bald Head Island. Olsen Associates, Inc. 2618 Herschel St., Jacksonville, FL 32204. 69 pp plus app. (August 2011). Olsen Associates, Inc. (2012). "Bald Head Island, N.C. Beach Monitoring Program Report No. 10 (May 2011— May 2012)", Report prepared for Village of Bald Head Island. Olsen Associates, Inc. 2618 Herschel St., Jacksonville, FL 32204. 70 pp plus app. (July 2012). Olsen Associates, Inc. (2013a). "Shoreline Stabilization Analysis", Report prepared for Village of Bald Head Island. Olsen Associates, Inc. 2618 Herschel St., Jacksonville, FL 32204. 338 pp. (July 2013). Olsen Associates, Inc. (2013b). "Bald Head Island, N.C. Beach Monitoring Program Report No. 11 (May 2012 — May 2013)", Report prepared for Village of Bald Head Island. Olsen Associates, Inc. 2618 Herschel St., Jacksonville, FL 32204. 63 pp plus app. (August 2013). Olsen Associates, Inc. (2014). "Bald Head Island, N.C. Beach Monitoring Program Report No. 12 (May 2013 — May 2014)", Report prepared for Village of Bald Head Island. Olsen Associates, Inc. 2618 Herschel St., Jacksonville, FL 32204. 63 pp plus app. (August 2014). Olsen Associates, Inc. (2015). "Bald Head Island, N.C. Beach Monitoring Program Report No. 13 (May 2014 — May 2015)", Report prepared for Village of Bald Head Island. Olsen Associates, Inc. 2618 Herschel St., Jacksonville, FL 32204. 65 pp plus app. (June 2015). Olsen Associates, Inc. (2016). "Bald Head Island, N.C. Beach Monitoring Program Report No. 14 (April 2015 — April 2016)", Report prepared for Village of Bald Head Island. Olsen Associates, Inc. 2618 Herschel St., Jacksonville, FL 32204. 80 pp plus app. (June 2016). Olsen Associates, Inc. (2017). "Bald Head Island, N.C. Beach Monitoring Program Report No. 15 (April 2016 — May 2017)", Report prepared for Village of Bald Head Island. Olsen Associates, Inc. 2618 Herschel St., Jacksonville, FL 32204. 80 pp plus app. (June 2017). Olsen Associates, Inc. (2018). "Bald Head Island, N.C. Beach Monitoring Program Report No. 16 (May 2017 — May 2018)", Report prepared for Village of Bald Head Island. Olsen Associates, Inc. 2618 Herschel St., Jacksonville, FL 32204. 69 pp plus app. (July 2018). Sept. 2018 - 18 - olsen associates, inc. APPENDIX A PLOTTED BEACH PROFILES WEST BEACH AND SOUTH BEACH September 2018 N O 00 'j 0 m O DC Q H H Q " O m O Oc 0 0 0 0 0 0 0 0 0 cV r-1 r-1 cV M ::I- Ln l0 I I I I I I (dn9N-Iaa3) uoLIena13 OOVZ 00£'Z OOZ'Z OOVZ 000'Z 006'T 008'T OOL'T 009'T v OOS'T v OOti'Z v V) 00£'T m E OOZ'T v OOT'T Ln 000'T 0 0 006 N 008 0 00/ 009 OOS OOti 00£ OOZ OOT 0 0 0 0 0 0 0 0 cv c i m (dn9N-100j) uo •en013 Figure A-01: Measured beach profiles at baseline Station-018+72, Bald Head Island, N.C. 008 OSL OOL OS9 009 OSS OOS LL v c OSti CO E OOti o OS£ 0 0 00£ 0 OSZ OOZ OSZ OOZ OS 0 July 2018 A-2 olsen associates, inc. N N + O m O DC Q H i " O " m O Oc 0 0 0 0 0 0 0 0 0 cV r-1 r-1 cV M ::I- Ln l0 I I I I I I (dn9N-Iaa3) uoLIena13 OOVZ 00£'Z OOZ'Z OOVZ 000'Z 006'T 008'T OOL'T 009'T v OOS'T v OOti'I v V) 00£'T m E OOZ'T v U OOT'T N 000'T v 006 N 4- 008 0 00/ 009 OOS OOti 00£ OOZ OOT 0 0 0 0 0 0 0 0 cv r N m (dn9N-100j) uo •en013 Figure A-02: Measured beach profiles at baseline Station-014+72, Bald Head Island, N.C. Oss 008 OSL OOL OS9 v OSS - v c OOS CO E OSti o OOti 41 OS£ r- V) 0 00£ OSZ OOZ OSZ OOT OS July 2018 A-3 olsen associates, inc. EVA 0 SOFA MONONA MEMER SOMERS MMMM11 SNEER 001101 MMEM11 MEMERIM Soong MMINUM NONNI Monson MMIFAMM SEEMS MOINES MEW KIMONO R81111 ME 0 0 0 0 0 0 0 0 0 0 rV r-1 r-1 r-4 m ::I- Ln CO I I I I I I WARN-,aa3) uoLlena13 oos'z OOti'z 00£'z OOz'z OOT'z 000'z 006'T 008'T OOL'T v 009'T v OOS'T v 00VT m E 00£'T v OOz'T �_ 00VT v 000'T N 006 008 OOL 009 OOS 00ti 0O£ 00z o0T I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I 1 1 1 1 I I I I 1 1 I I � I I I I I I I I 1 I � I _O_ S_ LL d) J C1� C% F- ii a7 `ao In f= O 53 O 1 • � 1 1 1 I I I I , I I I 1 L o Ci r� �> c-I O N O N CJ Cf) N f`J r, <U a) -0O U) O s) O N N -D N <U (W O ? O O c, Z Q 0C G- C_ 1 1 1 I I L I L ' O O O O 0 0 0 N r-1 r-1 N m I I I I WARN-1aaj) uo •en013 Figure A-03: Measured beach profiles at baseline Station-012+00, Bald Head Island, N.C. 006 058 008 OSL OOL OS9 v 009 - Oss m E OOS 0 OSti 41 0 OOti c- 0 OS£ 00£ OSz 00z OST OOT July 2018 A-4 olsen associates, inc. 009'Z OOS'Z OOti'Z 00£'Z OOZ'Z OOVZ 000'Z 006'T 008'T v OOL'T v 009'Z •v In OOS'T m E OOt7'T v U 00£'T N 7 OOZ'T L OOT'T N 000'T O 006 008 OOL 009 00S 00V 00£ OOZ 0 0 0 0 0 0 0 0 0 cV r-1 r-1 (V M ::I- Ln l0 I I I I I I (dn9N-Iaa3) uoLIena13 I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I t= O _3 f" +n O _ p U 12 cs M L) I I "' �> ��= ci > i ct �i N CJ frl v -LE <5 a� i s) J N N S) N E� (`J y • 10 ••� I I 1 I I 1 I • ' I L L • O O O O O O O c-j r-1 N m I I I I (dn9N-100j) uo •en013 Figure A-04: Measured beach profiles at baseline Station-008+00, Bald Head Island, N.C. 000'T OS6 006 058 008 OSL v OOL L.L v c OS9 m CO 009 v U C CCS OSS 0 L OOS N July 2018 A-5 olsen associates, inc. only, m t 00 MER I son 0 son son 1 SEEMS MEMMEM Solon NOISOME solos Solon OMENS MEMEM11 Solon MMIMMIN MEMEMI MONONA SEMMES monvid SERUMS ONION MrIMMEM 0 0 0 0 0 0 0 0 0 rV .� .� rV m ::I- Ln (0 WARN-,aa3) uoLlena13 009'Z 005'Z OOti'Z 00£'Z OOZ'Z OOT'Z 000'Z 006'T 008'T v OOL'T v 009'Z •v OOS'T m E OOti'T (U 00£'T OOZ'T 0 00VT N 000'T O 006 008 00/ 009 OOS 00V 00£ OOZ 0 0 0 0 0 0 0 N N m WARN-100j) uo •en013 Figure A-05: Measured beach profiles at baseline Station-004+00, Bald Head Island, N.C. 000'T OS6 006 058 008 OSL v OOL L.L v c OS9 m 009 v c OSS V) 0 v OOS N OSti W1 July 2018 A-6 olsen associates, inc. SU 00 MEN' son, SEEMS monsoon Monson MONSOON Emmons 0010091, ONESS11 00100111 Solon I 001001 0010011 moons ONINESE SOMENJ SOOPWAAS 0 0 0 0 0 0 0 0 0 rV (� (� r-4 M ::I- Ln (0 WARN-,aa3) uoLlena13 AI 1 • 4 7 005'Z f= +i 7 OOt7'Z ° U U _3 ((n C) U O N i3 j U i3 f� fl L ,n f2 O i +-' U<) �� U OOZ'Z �_ o O N U O i+ (n S_ Y OOZ Z O 000 v O o +' o� U (7 i O f� O N S= O+�t f_ `y +i f_ o a g L c0 L O N O O N O (D N O a7 `i N 0 (Yl 006'l Q/ S) o N v S) C) v N -. r, ' <u S) a) ') n3 J 008 T V O L. = Q O Z O_ Q O U Z O �3 0 4- a OOL'T (U v 009'l; •� I I � � V OOS'T m E i OOti'T v U ' 1 OO8'T , OOZ'T OOT'l N o 0?. 000'T 006 r,, , 008 / OOL 009 OOS 00V '. ' '. . 00£ = 3 OOZ 0 0 0 0 0 0 WARN-100j) uo •en013 0 Figure A-06: Measured beach profiles at baseline Station 000+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) OSO'T 000'T OS6 006 058 008 v OSL L.L v c OOL m OS9 0 v U C 009 0 v OSS N Al u July 2018 A-7 olsen associates, inc. 1: an 00 son monsoon SOMEONE Solon monsoon, solos Monson OMENS 00100111 Solon 0010011 0010011 100151 ONEOF 00101100 0010FA ONO&O SPAIMEN WAI aim 0 0 0 0 0 0 0 0 0 rV .� .� rV M ::I- Ln (0 WARN-,aa3) uoLlena13 009'Z OOS'Z OOti'Z 00£'Z OOZ'Z OOT'Z 000'Z 006'T 008'T v OOL'T °v' 009'T OOS'T m E OOt7'T v 00£'T OOZ'T OOT'T N 000'T O 006 008 OOL 009 00S 00V 00£ OOZ 0 0 0 0 0 0 0 r14 � � N m WARN-1003) uo •en013 Figure A-07: Measured beach profiles at baseline Station 004+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 000'T OS6 006 OS8 008 OSL v OOL L.L v c OS9 Ln CO 009 v c OSS V) 0 v OOS N OSti 00V OS£ 00£ OSZ ON Al July 2018 A-8 olsen associates, inc. '101 1: 0 00 son son MEMMEM monsoon Monson MEMMEMMIN, SEEMS MONSON OMENS I MEMEM11 ONION 1 MMMMMj INNER"] OMENS , MEMMUM EMMONS songs MICA ISFAAMME O O O O O O O O O rV r-1 r-1 r-4 M ::I- Ln (0 WARN-,aa3) UoLTena13 OOs'Z 006 1 OOVZ C •- f- OSO OO 7 OOPZ �� �� U M ° U I C) O 4J i- O U L� E I 0O1.77 Z RS �-. RS yj- U ++ C: O F- 42 ! O 008 OOVZ O CL 0 vi CL w O CL CI 6 i N d O c= 1 2-1 U F7 �� O U - o a r• ci;_ N U ii O a7 f- to O O S L 77 v N LS c 006'l o vl a' d; f- C O °> O ri O 2 OOL o o 0 q) 00 0 o N I fV u N o C) OO8' T L � N S1 o �� a) o Sj ai 0 O ti0 T O59 OOL T .-. z a: O z CL O a: z ti C) 2 z- 2 009'T I I 009 v oos'l oss ru oot7'T m ; ; ro m E E OOCT ° 00s U ; ; i U OOZ'l; r C Ln Osv 00T,T I I I I o OOO,T / OOti N c- o I I I 4- o 006 OS£ 008 I I OOL 00£ 009 I I ' OSZ OOS I� 00-V ... ............. ... OOZ OOE I� OSZ OOZ =3 ooi OOT O O O O O O O N r-1 r-1 N m IZT WARN-100j) Uo •en013 Figure A-08: Measured beach profiles at baseline Station 008+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) July 2018 A-9 olsen associates, inc. k kiss 0 SOME MEMMEM MEMMEM Monson monsoon Emmons MMMMMM MMMMMII MMMMMIJ MMMMMI MMMM14 001001 MONONA MEMER MONFAM ONE SEASON WIN 0 0 0 0 0 0 0 0 0 rV .� .� r-4 M I- Ln (0 WARN-,aa3) uoLlena13 00s'Z OOti'Z 00£'Z OOZ'Z OOT'Z 000'Z 006'T 008'T OOL'T v 009'T v OOS'T OOt7'T m E 00£'T v OOZ'T OOT'T 000'T N 006 0 008 OOL 009 OOS OOti 00E OOZ OOT O U :3 O M O U () U vi 00 >3 U LS C) 0) L l7 ui o �i a ci V ) Q QX CL a+ v{ O ��'1 c N v O_ iSi O~ 12 0 `C o o O of �> I, 4 a' , a N = e_ u, [; .... p 0-- p a o a c o o N dl N o �� N �0 �--� 00 0 v N CY) O L O N O QI Lf1 (U N n C) W o �? `ci o" m o Si o a O Z c! I � r i f i i r r- yr r _ IF , ... �.. �. �... ... ... .. . = 3 0 0 0 0 0 0 0 N N m � WARN-100j) uo •en013 Figure A-09: Measured beach profiles at baseline Station 012+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 006 058 008 OSL OOL OS9 009 - OSS m E OOS 0 OSti V) 0 OOti c- 0 OS£ 00£ OSZ OOZ OST OOT July 2018 A-10 olsen associates, inc. his OVE 0 0'a EL on 0 son Emmons Emmons monsoon monsoon, SOMEONE I Monson SNISSGWI'' SEEMS MONSON ONSONFA SENSES snoop] SONSIS SOMPAS ONFUS ONFASSE OMAN am ME E 0 0 0 0 0 0 0 0 0 rV r-1 r-1 rV M ::I- Ln (0 WARN-,aa3) uoLlena13 00-V'z 008 r 00£'Z 2 2 OSL OOZ'Z -. -. ° o ° I 0oT Z '" �i rti o o 001 v@i .-. v@i a~', Q. v@i Q. p U 000'Z F N F I I rl 0 � 0 Lf1 N 0 0� LI u C: N ate.+ a° C � a OS9 006'Z v o v a. 2 s t a N N a c: b a; p - a O N - o 008'l o a° vl a; 009 0 o a �1 ao 0 0 OOL'T O v Lf1 QI CI N ;,00 E S' C' O N T N ? OSS 0091l z° a z° a:` z c; z OOS'T °� l i i 005 v OOti'l In OSV N 00£'T CO m E i E OOZ'T i r OOti 1 1 c� � / U OOT'l ra 1 1 /� M OS£41 000'T 1 1 r O 006 ' O 00£ 0 1 �' 4- 008 1 , ', ' ° ' ' �% ' osz OOL �1 009 OOZ / - o0S , ; OST 00-V , ,1 •1 oo£ 1 Doi 00z 0S OOT =3 0 0 O O O O O O O r1A r-1 r-1 N m WARN-100j) uo •en013 Figure A-10: Measured beach profiles at baseline Station 016+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) July 2018 A-11 olsen associates, inc. —F 1: --Is 0 monsoon monsoon SONESS SEEMS Monson Emmons Emmons SONSOM INSINFA SENORS SONSFAS Solffm SEERNES ERFAVAS ONIONS SMAS 0 0 0 0 0 0 0 0 0 rV r-1 r-1 r-4 M ::I- sn (0 WARN-,aa3) UoLlena13 oo-V'z oo£'z OOZ'z OOT'Z 000'z 006'T 008'T OOL'T 009'T Q1 OOS'T v OOVT 00£'T m E OOZ'T v OOT'T 000'T 006 N 008 OOL 009 OOS OOti 00£ OOz OOT 0 0 U c c 0 C U U U i v O Ul E. O S:i O 5 O a i °! of U O U CL u�i O�. s!s N <) 1 o o 0 0 � �� M 4 u uu N U u u z O 0 O� a / 0.o Q N NI C, `ci a o o" o / O O v �I O O l0 00 CM,M N 0 1 �, N�� O fOJ ` E N E', Ci E � S] £_ O N vYi 3 N C —. N rd O °J O 3 0� Ci. O u �s U Z Q z< Z O c_ A ,•1 �I I 1 y/ it ..,............. =3 O O O O O O O WARN-100j) Uo •en013 Figure A-11: Measured beach profiles at baseline Station 020+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 008 OSL OOL OS9 009 OSS 00S LL OSV CO E 00-V OS£ 41 0 OSZ OOZ OST OOT OS 0 July 2018 A-12 olsen associates, inc. is kwo ELF, offit 0 IMMEP SEEMS monsoon Monson NONSENSE NONSENSE MONOSSON MONOSSON SEEMS son INNER MINOR Moorafin MWAINEM mignon Nilson MIAMME Olson A�ONI ME 0 0 0 0 0 0 0 0 0 rV r-1 r-1 rV M ::I- Ln (0 I I I I I I WARN-,aa3) uoLlena13 00-V'z 00£'z OOZ'z OOT'z 000'z 006'T 008'T OOL'T 009'T v OOS'T v OOti'T v 00£'T m E 00z'i v 00T'T 4-1 000'T v 006 N 008 0 OOL 009'' 00S 00ti 00£ 00Z OOT 0 I I I I I I I I I I I 1 I I I I ' I I I I I I I I I 1 r I / •/I I / II I I / / I I I I I I I I I I I I 1 I C 1 I 1 I 1 1 I 1 / 1 0 u i O O I i I I f0 f0 O" •U C H C U U N- O O C F H L I N U 0 rl l!1 i a+ a . N O N d H 7 � 2 N N = L L 1 1 i i L O O N O 1 I N ON oo CN cD cL-I O O I I cD Y ON E 4 ON E N T T • 1. I• • Z a Z a Z O 2 Z 2 0 O O 0 0 0 0 I 1 WARN-100j) uo •en013 Figure A-12: Measured beach profiles at baseline Station 024+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 008 OSL OOL OS9 009 OSS OSti m E 00-V OS£ 41 0 0sz OOZ OST OOT 0S 0 July 2018 A-13 olsen associates, inc. "INS 4W 0 1 Me 00 4=1 ski 4001 ME ski OR 0 MEN' MONSOON SONESSIT" Monson SEEMS monsoon Monson ONENESS Emmons SONSOOF SONSER NOODUMN SERUMS Ordmom Nilsson OPMENES man EVANSON Fam ME1111 0 0 0 0 0 0 0 0 0 0 rV .� .� rV M ::I- Ln (0 WARN-,aa3) UoLlena13 00s'Z OOti'Z 00£'Z OOZ'Z OOT'Z 000'Z 006'T 008'T OOL'T v 009'T v OOS'T v OOt7'T m E 00£'T v OOZ'T OOT'T 000'l N 006 008 OOL 009 OOS OOti 00£ OOZ OOT I I , , I •1 I/ OF I ♦ ' I • •1 1I I 1, Z/1 I ' ♦ I I I ♦I I I • I I ' I 1 ' I 1 I I 1 1 � 1+ 1 1 1 1 1/ 1 1 /1 1 1 � 0 u C C O U O l i 1 I 1 1 u � u h 2 N U aL+ Y � aL.. C7 to to fl' u c H c 0 0 o 2 g o 0 0 U U n I 1 I 1 N- O O C H ♦? L 1 1 a+ O i o o ao 0 � H N = L L 1 1 i i L C N 1 I O O o 0 1 I ON N ON ~O oo ON o N O N N N 1" N 00 E a. E ON E 4 ON E N 1 1 i I o T T Z Q Z Q Z O 2 Z 2 0 0 0 0 0 0 00 I 1 1 WARN-100j) Uo •en013 Figure A-13: Measured beach profiles at baseline Station 028+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 006 OS8 008 OSL OOL OS9 v 009 - OSS m E OOS 0 OSti 41 0 OS£ 00£ OSZ OOZ OST OOZ July 2018 A-14 olsen associates, inc. kin 91 MA or SEEMS son on s Monson SEEMS MEMMEMEWMONOMER t Emmons I I monsoon MMIMMEW so MEMO MONZA EFFAMEM MrAfills SIRENS spin son 0 0 0 0 0 0 0 0 0 rV r-1 r-1 rV M ::I- Ln (0 WARN-,aa3) UoLlena13 00S'z 00-V'z 00£'z OOz'z OOT'z 000'z 006'T 008'T OOL'T v 009'T v OOS'T v OOt7'T m E 00£'T 41 OOz'T �_ OOT'T v 000'l N 006 0 008 OOL 009 OOS 00ti 00£ 00z OOT I 1 " I 1 , •, r I 1 , r 1 1 I 1 1 � � • I 1 / I 1 ' I 1 I 1 , I •I ,, i 1 1'• f J 1 I I 1 I If I f I •f n I / 1 1 � 1 1 I I I I 1 1 1 1 y 1 Q � 1 I u u 2 0 2 to to fl' u c H c. a' 8 °o' o a 1 I i N i t 1 I cO 0 c ca' Op d g L L. 1 I c�-I o o v o a oo 0 0' N N N O V N to 0 Z Q Z Q Z O Z �. � • I I I � � , 1 1 O O O 0 0 O 0 I 1 1 WARN-100j) Uo •en013 Figure A-14: Measured beach profiles at baseline Station 032+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) OS6 006 OS8 008 OSL v OS9 - 009 Co E OSS o OOS 41 0 OSti c- 0 00V OS£ 00£ OSz 00z OST July 2018 A-15 olsen associates, inc. oil 0 MOVE MONSOON MONSOON mossomm sommon SEEMS SOMEONE OMENS OMENS I ONION sommono ONION SOMIUM NORM MRIMME MrAm Nilsson ORIN PA WEEM 0 0 0 0 0 0 0 0 0 0 rV r-1 r-1 rV m ::I- Ln (0 I I I I I I WARN-,aa3) UoLlena13 00s'z OOti'z 00£'z OOz'z OOT,z 000'z 006'T 008'T OOL'T v 009'T v OOS'T v OOti'T m E 00£'T v OOz'T 4-1 OOT'T 000'l N 006 0 008 OOL 009 OOS OOti OOE OOz OOi I I I I � I I ' I I ' I I I' , I I ' I I � I I r I I I I I I ' , , I I I I , I 1 I 1 '. , 10 I 1, • I I V I �n , I 1 , r• •I I 1 •I 1 I T I I I � I I I I I I I a u 2 c 3 I U + t + I d O O u O o N C nl M I N I� Q1 W O I I I I I j Z 0 Z I I I I � I I 2 I ' L L C C 0 0 0 0 0 I I I 1 WARN-1aaj) Uo •en013 Figure A-15: Measured beach profiles at baseline Station 034+00, Bald Head Island, N.C. OS6 006 OS8 008 OSL v OS9 - 009 m E OSS o OSti 4- 0 00v OS£ 00£ OSz OOz OSi July 2018 A-16 olsen associates, inc. Lis MA MIA ON 0 MM11 MMMMM! SEEMS son SEEMS MEMMEM Monson EMMEMME Emmons MOMMEN's IMEMEME MMIMMU_ MMMMrA MMERA, MERNIM EVAN OWNS 0 0 0 0 0 0 0 0 0 0 rV r-1 r-1 rV M ::I- Ln (0 I I I I I I WARN-,aa3) uoLlena13 00s'Z OOti'Z 00£'Z OOZ'Z OOT'Z 000'Z 006'T 008'T OOL'T v 009'T v OOS'T v OOt7'T m E 00£'T v OOZ'T Ln OOT'T v 000'l N 006 0 008 OOL 009 OOS 00ti 00£ OOZ OOT I I I I , , I I I I I 1 I I I I I �A I I I I I 1 I I � I I , I I ✓ I I I I I I I fP0 I I w I 1 I / I C r o o 0 y I ' u u W i V i F c i N a O °o. @ a C' O o U I I o 0 0 t I - 2 U I I o o r a o a N O N a a? Lo I I o - o I I I CD 0 NO ei N O N .-I � N m a W E ♦+ E N E, O E O 1 I > M > — > O T j T 0 0 Z Q Z Q Z O Z 1 I I 1 I I �• 0 0 0 0 0 0 00 I I I 1 WARN-1aaj) uo •en013 Figure A-16: Measured beach profiles at baseline Station 036+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) OS6 006 OS8 008 OSL v OS9 - 009 m E OSS o OOS 41 0 Osti C 0 00V OS£ 00£ 07Z 00Z OST July 2018 A-17 olsen associates, inc. � A 0 ski 0 not] SEEMS SEEMS Solon MEMMEM SOMEONE soon 0 OMENS SENSE Monson INS OMENS NOISE MMMMAAM MMIRAM SIGNS MRMM MWIMME F, P 0 0 0 0 0 0 0 0 0 rV .� .� rV M ::I- Ln (0 WARN-,aa3) uoLlena13 00s'Z OOti'Z 00£'Z OOZ'Z OOT'Z 000'Z 006'T 008'T OOL'T v 009'T 010S'i ra ooi7'T co E oo£'T v OOZ'T 4�_ OOT'T v 000'l N 006 0 008 OOL 009 OOS 00ti 00£ OOZ OOT I I , I I I I , 1 1 1 I I I I , I I , I I , I I ' ' I I , . I I I , I I ♦ � I I 1 ♦ � I I I I 1 , I 1 I 1 • I , 1 , • I 1/ I I,� I `♦ II C U _ ♦p`+ �2+ n o y0 ' I ♦ �' ♦ I I -0'. o � 0 Y O CD ~ � O C' O d R m N N H N 0 N N I 1 R > R 1 , , Z Q Z O Z 0 0 0 0 0 0 00 I I 1 WARN-100j) uo •en013 Figure A-17: Measured beach profiles at baseline Station 038+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) OS6 006 OS8 008 OSL v OS9 - 009 co OSS OOS 41 0 OSti c- 0 00V OS£ 00£ OSZ 00Z OST July 2018 A-18 olsen associates, inc. IV oil oil oil 0 Not Emmons sonsom NNINNER, Emmons I " sonsooff, soloost, Emmons monsoon SONOMA solow(v r em NNINFAI NNERWAAM smu""A-r'so Orions, ORFAI'Moss Nilsson PFF 0 0 0 0 0 0 0 0 0 rV .� .� rV M ::I- Ln (0 WARN-,aa3) uoLlena13 00-V'z 00£'z OOZ'z OOT'z 000'z 006'T 008'T OOL'T 009'T v OOS'T v OOti'Z v 00£'T m E OOZ'T v OOT'T 000'T 0 v 006 N 008 0 OOL 009 00S 00ti 00£ 00Z OOT 0 I I � fill,. ' I I 1 1 YA � r „ I 1 , r � 0-4 / 1 1 1' 1 Ili 1I I 1 ' I J�, I � l I 'r 1 1 11 I I J I O O 1 1 1 I R C W L U Y U, c F c o o m N U � t 1 1 O e-I O F j d O d N O N oo N n0VI No. 9 N C' W E ♦+ E N E' NO E N I 1 > M > — > O 0 A z° a' z° a z° I 1 1 I 3 1 3 I I i �• 0 0 0 0 0 0 00 I 1 WARN-100j) uo 'en013 Figure A-18: Measured beach profiles at baseline Station 039+60, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 008 OSL OOL OS9 009 CAW OSV M m E OOti o OS£ 41 0 00£ r- 0 OSZ OOZ OSZ 001 0S 0 July 2018 A-19 olsen associates, inc. 1: oil] Ln oil + f < ME ME V) on MMISOM MMISOM SOMMEM MMISOM SOMEONE MMMMIM MMIMMIA MEMMODE Mosorra MMEW5111 Moorms MORRIS ONFAIN MKIMME OMENS Nilsson MAE ifs WEEM 0 0 0 0 0 0 0 0 0 rV .� .� rV M ::I- Ln (0 WARN-,aa3) uoLlena13 00z'z OOT,z 000'z 006'T 008'i OOL'T 009'T OOS'T OOti'T v 00£'T v OOZ'T v OOT'T m E 000'T 41 006 008 LJ OOL N 009 O OOS 00V 00E 00Z OOT 0 OOT- OOZ- 1 I � , I I � I . I � Jq ► 1 I ,i ►. I 'I . ► 1 / 1 1 y �► 1 I II 1' 1 , 1 1 i 1 •I � 1 I I /1 I O O � +�+ ♦+ aL-+ Ur o n o O ~ O u o u 1 I ti c v l7 0_ l7 0 0 o c Y U O L 1 I yy n1 I a O O O N e-I 00 NC> M ON 0 N w N N N d ► 1 1 I — z a z o zo 1 I I = 3 I i � • l l l l 0 O O 0 0 0 00 I 1 WARN-100j) uo •en013 Figure A-19: Measured beach profiles at baseline Station 041+50, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) OS9 009 OSS OOS OSt7 00V v OSE - 0 S T OOT OS 0 OS OOT- OST- July 2018 A-20 olsen associates, inc. 0101 oil ME se on 0 most, Monson SMISSER Monson sonsoor sonsoor 00100X smosorl SOMER,"Arl 0010011AM SMIRA SENFAMS smfflams SIFFISS SPASSE Simmons SWISS FAINESS 0 0 0 0 0 0 0 0 0 rV .� .� rV M ::I- Ln (0 WARN-,aa3) uoLlena13 OOE'z OOZ'Z OOT'z 000'z 006'T 008'T OOL'T 009'T OOS'T v OOti'T v 00£'T v OOZ'T m E OOT'T v 000'T 4-1 006 v 008 N OOL O 009 OOS OOti 00E OOZ OOT 0 OOT- IT -, I, , M� / 1 •� I I' I' O o� I .. 5 . O— O 81 0 o C H a H V a+ t « a° ro i E E E ry E a n E ry i ' w w w o w> o i z i zw a' z° a zw III Ln 0 Ln 0 Ln 0 Ln (dn9N-100j) uo •en013 Figure A-20: Measured beach profiles at baseline Station 043+47, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) OOL OS9 009 OSS OOS OSti v 00V U- OS£ CO OOZ OST OOT OS 0 OS- 001;- W July 2018 A-21 olsen associates, inc. on on I son looms moons MOMMEM moons ' MOMMEN MMMMP)j MMMFIM MMIWAM EM11011 ONFAIME Mgrgoo Ellison MWAMME ONIME Milan 0 Nilson IMM 1111111 MM 0 0 0 0 0 0 0 0 0 rV r-1 r-1 rV M ::I- Ln (0 I I I I I I WARN-,aa3) uoLlena13 oo£'z OOZ'Z OOT'z 000'z 006'T 008'T OOL'T 009'T OOS'T v OOti'T v 00£'l; v OOZ'T m E OOT'1 0 v 000'T 006 v 008 N OOO L 009 00S OOti 00£ OOZ OOT 0 OOT -40 1 1 1 1 , , I r 1 1 / 1 1 / 1 1 1 1 1 f 11 1 11 I ' 1, 1 LI 1 II , I I I I I � I I 1 1 I 1 II 1 0 0 i � Y r 0 1 r 1 = O c N F 1 F ooy�dod N O L L I 1 1 ry ti ry O ti ry M ti E N E N E N 1 Z Q Z O 9 Z 9 I 1 I Ln O Ln O In O Ln (dn9N-100j) uo •en013 1 1 Figure A-21: Measured beach profiles at baseline Station 044+25, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) OOL OS9 009 OSS OOS Ost OS£ CO OOZ Ln 4- OST OOT Os 0 Os- OOT- W July 2018 A-22 olsen associates, inc. ENNUI MOVIES MOVIE ONFAINE 0011100 SEASON OFAME ON son 01,1100 01111000 WAVE PA 0 0 0 0 0 0 0 0 0 rV r-1 r-1 rV M ::I- Ln (0 I I I I I I WARN-,aa3) uoLlena13 OOE'z OOZ'Z OOT'z 000'z 006'T 008'T OOL'T 009'T OOS'T v OOti'T v 00£'T v OOZ'T m E OOT'T v 000'T 4-1 006 v 008 N OOL O 009 OOS OOti 00E OOZ OOT 0 OOT- 1 1 1 ✓ 1 / / / I � 1 ► I � 1 / I 74 \ 1, • 1 1 I ► 1 � I I ►' ' I' ' 1 ► r I 1 /1 1 � I � 1 1 1 1 1 1 ► 1 I 1 ► 1 1 1 � I � 1 o�z 202 _ k o Y o n a« V p V gji G N IJ N 0 N � a° N O N 1 d L O Y z N v o 0 0 z° 4 z° o z° i I I I 1 ✓ � � I I I I � � I Ln 0 Ln 0 Ln 0 Ln (dn9N-100j) uo •en013 I Figure A-22: Measured beach profiles at baseline Station 045+07, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) OOL OS9 009 OSS OOS OSti OS£ CO OOZ Ln 4- OST OOT OS 0 Os- 001;- July 2018 A-23 olsen associates, inc. 0 0 0 0 0 0 0 0 0 cV r-1 r-1 cV M ::I- Ln l0 I I I I I I (dn9N-1aa3) uoLIena13 OOE'z OOz'z OOT'z 000'z 006'T 008'T OOL'T 009'T OOS'T v OOti'T v 00£'T v V) OOZ'T m E OOT'T o v 000'T 41 Ln 006 0 v L 0 008 N OOO L 009 00S OOti 00E OOZ OOT 0 OOT- le , y r 1 • , 1 r ► I OP 1 it1' •I I 1 I I/ I •'1 1 I � I. I� 1 / � 1 1 \ � \I 11 I / II 1 1 1 1 ►1 _ 0 ` U ` 1 fO io o 0 0 " 1 0 V V N V N a+ L a+ I 1 Vl C C I 1 1 O O O O N N C 1 N OM y O O d d 1 1 1 1 1 Z Q Z O Z 1 I I I I I g g I I I I I I Ln 0 Ln 0 Ln 0 Ln (dn9N-100j) uo •en013 1 1 Figure A-23 Measured beach profiles at baseline Station 046+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) OOL OS9 009 OSS OOS OSti 4-1 00V U- OS£ CO L O OOZ OST OOT OS 0 Os- OOT- July 2018 A-24 olsen associates, inc. 0 0 0 0 0 (V r-1 ri N (4n9N-1aa3) uoLIena13 00E'z OOz'z OOT'z 000'z 006'T 008'T OOL'T 009'T OOS'T v OOti'T v 00n v In OOz'T m E OOT'T o v 000'T 41 006 v L 0 008 N 1— OOL O 009 00S OOti 00E 00z OOT 0 01KOOIX 1 i 1 ' / / 1 1 1 J , 1 1 1 ,• 1 1 1 I �I � / 1 1 11 1 1/ 1 1 '1 1 1 11 I i 1 /1 1 /1 1 / 1 1 / 1 I I I 1 \ 1 I \ 1 I I I / 1 1 C L u I 1 V V a a '^ a o c W l7 l7 0 6 p N 0 H H I 1 L 0 u a« a a a 0= `o 0 n .w+ w roi m o � o a N a o a rv" m I 1 E E ry E E N E ON W w> p> o f i z a' zp a zp zp 1 1 I I 1 I I 3 � 1 1 = � g III111� 1n o L n o 1n 0 1n r-1 (dn9N-100j) uo •en013 I Figure A-24: Measured beach profiles at baseline Station 046+89, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) OOL OS9 009 OSS OOS OSti OS£ m OST OOT OS 0 OS- OOT- July 2018 A-25 olsen associates, inc. 1 , ooz'z 1 o 1 I , •, OOT'z o + � rn 1 000'z 1 1 1 1 , , 2 O 1 I 006'T F— ' 008'i Ln ' * OOL'T r 1 1 I 009T I I 1 OOS'T I I I ' OOt7'T it a-+ v I I LL OOVT v 1 1 In OOT'l; CO 1 1 E 000l o 1 1 1 1 , t , • Qi U 006 ' 008 1 I n o OOL N 4- 009 I Le �I I Z 005 I i O a 1n N OOti I I U m OOE I I I N 00 z I ' - � r a O Z 00T I I Z } W O I I O IIAii \ /� N 0 O I I I _ a OOZ- I H Z OOz- 0 0 0 0 0 (V r-1 ri N (4n9N-Iaa3) uoLIena13 I 1 , � I I I 1 I1 •,' 1 1 1 � � I I I � 1 ' ' /� 1 1 1 1 , N 1 1 ' 1 1 � 400 1 1 � I 1 ' I I I I 10 1 1 1 ' 1 1 1� I 1 , 10 • 1 , 000 I � , 1 1 a 10 L: U U O d FZ U t6 L L 0 0 a ' 1 1 1 I 1 ♦. O L. d c O O „I O a - QCD (V1 1. � 00 £ o E o 0 'd > T O o z O 5 z 1 1 1 1n 0 1n 0 Ln 0 Ln (dn9N-100j) uo •en013 1 Figure A-25: Measured beach profiles at baseline Station 049+00, Bald Head Island, N.C. OOT'T OSO'T 000'T OS6 006 v 008 .L v c OSL m CO v 0 009 N OSS 00S OSt7 oot? OSE 00E July 2018 A-26 olsen associates, inc. O O O O O (V r-1 ri N (4n9N-1aa3) uoLIena13 OOE'z I , OOz'z C 0 U I ► , ; OOT'z - N _ �, O _ u ai ul C U O i I I II a t S; 000'z N��i o�: N � ► • .-I a (D 0. (7 C. H '7 �i O [a} 006'T r�l 'y: o c- o I I • • ' L ?. S- L 008 I. v, til Ins �I a: �: � I • ►'t NI R Cc,NI SI IX1 I �1 a O N O V I I •/ 1 OOL'f a N N r SI n! a)oo �N , I • N� Ei LI RI 4 009'Z O� CL C � �: c �, _ G I I •` 005 T I I I v OOti'T v I I i a Iv 00£'T v I V) OOZ'T m f E I 00T'T I / u 41 006 O 008 t Ln • / �/ •� 009 OOS I, OOti 1 � • I 00E 1 I 1 ► OOZ a II OOT ( 1 9 13 0 1 i 3 L L OOT I (dn9N-100j) uo •en013 Ln r-I Figure A-26: Measured beach profiles at baseline Station 050+50, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) OOT'i OSO'i 000'T OS6 006 v 008 Li v c OSL M 00 �y v 0 009 N 4- OSS OOS OSt7 00V OSE ON W1 July 2018 A-27 olsen associates, inc. 'ILn 0 0 0 0 0 (V r-1 ri N (4n9N-Iaa3) uoLIena13 OOE'z OOz'z OOVZ 000'z 006'T 008'T OOL'T 009'T OOS'T v OOti'T v 00£'T v OOZ'T m E OOT'T v 000'T D 006 v 008 N OOL O 009 OOS OOti 00� OOZ OOT 0 OOT- 1n 0 1n 0 Ln 0 Ln (dn9N-100j) uo •en013 Figure A-27: Measured beach profiles at baseline Station 051+00, Bald Head Island, N.C. OOT'T OSO'T 000'T OS6 006 v 008 L.L v c OSL CO v 009 N OSS W1 July 2018 A-28 olsen associates, inc. Ell I Kai, MEP no" mmot MMEL MMKI MMEN) MME1 mmal mmat mmmll MMM-1, MME&I MMFAII MML91 WIN'dr-KNA PA MiVAM We 0 0 0 0 0 (V r-1 r-1 N (4n9N-1aa3) uoLIena13 oOCZ OOZ'Z OOT'Z 000'Z 006'T 008'T OOL'T 009'T OOS'T v OOti'T oon v OOZ'l o OOT'T v 000'T 4-1 006 LJ 008 N OO0 L 009 OOS 00ti OOE o0Z OOT 0 OOT- I 1 � ' ► 1 1 � I I •, I � 1, / •; / I 1 , • 1 / 1 1 1 I , I I I I I I I / I I / I I I I / I / 1 1 I 1 O O I 1 a I 1 1 Oo p . p N p H L H O ti V C u a o a 0 0 6 -0- N O N I « a« a o= o a I 1 1 N ON 0 w N M O O O a N L p a ry .i ON I E E E ry E a N E N > O T > T z a' zp a zp o i z i g g IIII��� 1n 0 L n 0 Ln 0 1n r-1 (dn9N-100j) uo •en013 I Figure A-28: Measured beach profiles at baseline Station 052+64, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) OSL OOL OS9 009 OSS v OOti m E OSE o OSZ r- 0 OOZ OST OOZ OS 0 OS - July 2018 A-29 olsen associates, inc. OOE'z O 1 1 1 I , 1 OOZ'Z O1 + 1 OOVZ I ^ — • 1 I LLr) O 000'Z — 1 I I — 006'T ' 1 I 008'T 1 1 I I OOL'T I I I I 009'T I ' OOS'T .-. ' I 1 — OOti'T 1 I v 00£'T v 1 ' I In OOz'T CO 1 I 1 1 E 1 1 I OOT'T 1 I 000'T to 1 I ' 006 1 I I I ' 1 008 N ' O OOL 1 I,, OLn 009 a N 00S U m OOV 1 LU 00E Oz 00Z r Z W> O 00T lop, W N O CC a 0 ' I Z 00T- I I I 1 I ICI 1 � � II ' I 1 / I I I I+ I I 1 I1 1 I 11 I 1 1 %I I � I I 1 � I I s 1 I 1� do ♦ 1 -1 1 I 1 1 y 1 , • 1 i 1.0 1 1 I 1 • 1, I ! I I I I I I I 1 I I I 1 I 1•' 1 I 1 I I O C' C Y O _ t o C N i 8 i I I O •U C'. F' C N I ` O a- O ' V' U 17 F L a. Q d I I 1 i C' ry C O O O N G Q O E cm 00 e: RD O ,. ° � zoO z I I Ii I I I ♦1 • � = 3 1 I 1 I 1 I 0 0 0 0 0 Ln 0 u1 0 1n 0 1n (V r-1 ri N r I r I r-I ri (4n9N-Iaa3) uoLIena13 ((In9N-Iaaj) uo •ena13 Figure A-29: Measured beach profiles at baseline Station 054+00, Bald Head Island, N.C. OSL OOL OS9 009 OSS 'Iim v OSV °LLs as c 00V CO OSE o OSZ 0 OOZ OSZ OOZ OS 0 OS - July 2018 A-30 olsen associates, inc. Ell I El, iM 6 NIP iMENEM 0 0 0 0 0 (V r-1 r-1 N (4n9N-1aa3) uoLIena13 oOE'z OOZ'Z OOT'Z 000'z 006'T 008'T OOL'T 009'T OOS'T v OOVT v 00£'I v OOZ'T m E OOT'T v 000'I 006 v 008 N OOO L 009 OOS OOti 00E OOZ OOZ Cd 0 ` OOT- 1 1.0 ' ► s 1 yI I oro — 3 a a .. o o 1 , •-I O F L O 1 1 1' � '• d i+ d '� L C � C ode Z; ,, E 1 ,/l y O y � y N I� y Op E- ENE��EN •/ I Z Q Z Q 2 O Z II�, l� 1 1 '1 �/ 1 ..,i �4 '• i i • oil �/ 1 � � � i � � � � � � � � � � 1 1 1 I 1 1 1 1 1 1 1 1 1 1 1 1 1 1 ->T = 3 1-1 FFTTTI-I I'l I I I I I I I I I I I I I 1n 0 L n 0 1n 0 Ln r-1 (dn9N-100j) uo •en013 Figure A-30: Measured beach profiles at baseline Station 056+56, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) OSL OOL OS9 009 OSS 'sIim v OSt7_ 00v CO E OSE o OSZ r- O OOZ OST OOT OS 0 OS - July 2018 A-31 olsen associates, inc. MONA MM MENEM MOMMIN 0 0 0 0 0 (V r-1 ri N (4n9N-1aa3) uoLIena13 oo-V'z OOE'zz OOZ'z OOT'z 000'z 006'T 008'T OOL'T 009'T v OOS'T v OOti'T •v 00£'T m i_ OOZ'T 41 OOT'T 000'T 006 N 008 0 OOL 009 OOS OOti 00£ OOZ OOT 0 I� 1 — 3 '2 0 , ri « �' c 1 j/ vf0i vf0i a•��. c a 1 i � /I o o n o 1 a a o o o C 0 1 / / M ' 4 •/ ) E E N E E O ' 11 Z Q Z Q 2 O Z 1 1, 1 • 1 � 1 1 1 1 , 1 ; 1 1 1 1 � 1 � � � 1 1 1 1 � 1 1 � � � � 1 1 1 1 \ � � � � 1 1 1 1 � = I 3 1n 0 L n 0 1n 0 1n r1 (dn9N-100j) uo •en013 Figure A-31: Measured beach profiles at baseline Station 060+51, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 008 OSL OOL OS9 009 Caw OOti o OSE 41 0 008 r- 0 OSZ OOZ OST OOT OS 0 July 2018 A-32 olsen associates, inc. MMV5 MMKIN MMWW-*'A ME, 0 0 0 0 0 (V r-1 ri N (4n9N-1aa3) uoLIena13 00S'z OOti'Z 00£'z OOZ'z OOT'Z 000'z 006'T 008'i OOL'T v 009'T OOS'T v OOti'T m E 00£'T o a, OOZ'T OOT'i 000'T N 006 0 008 OOL 009 OOS OOti 008 OOZ OOT o � , o r o r U � /• 0 p d � �• p ~ p 1 � / , I v�i v�i a a o .. c a a o o= o 0-0 E E N E E N ' Z Q Z Q 2 O Z I ��I,III / y i i Y• Y-7 (j, '✓ ... _. ... 3........... 2 2 In 0 1n 0 Ln 0 Ln (dn9N-100j) uo •en013 Figure A-32: Measured beach profiles at baseline Station 065+50, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 006 OS8 008 OSL OOL v 009 - OSS m E 005 0 OSti 41 0 OOti C 4- 0 OS£ July 2018 A-33 olsen associates, inc. oo-V'z 00£'z OOZ'z 00 V'z 000'z 006'T 008'T OOL'T 009'T v OOS'T v OOti'T •v V) 00£'T m E OOZ'T v OOT'T rcu: �_ 000'T 0 v L 006 N 008 0 OOL 009 OOS OOti 00£ OOZ OOT 0 0 0 0 0 0 (V r-1 r-1 N (4n9N-1aa3) uoLIena13 1 , p 0 1 P I 3 1 g o n 0 0 o m~ a~ N li a+ L ,+ � 1 •-I ,l, o s o N L O � a 1 1 �• , N O O1 � W N I� N 00 E « E G- a`i o- 0 N W W N O T T 1 Z Q Z Q Z O Z 1 '• „ O /i I � � IX � � 1 I' 1 , 4 1 1 1 1 1 I 1 1 l dP ' � � � � 1 1 1 1 1 1 = 3 1n 0 1n 0 Ln 0 Ln (dn9N-100j) uo •en013 Figure A-33: Measured beach profiles at baseline Station 069+46, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) Oss 008 OSL OOL OS9 v OSS - OOS CO E OSti o OOti Ln 0 L OS£ 4- 0 00£ OSZ OOZ OST OOT OS July 2018 A-34 olsen associates, inc. oo-V'z oo£'z OOZ'z 00 V'z 000'z 006'T 008'T OOL'T 009'T v OOS'T v OOti'T •v In ru 00£'T CO OOZ'T o 41 OOT'T 000'T 0 L 0 006 N 008 0 OOL 009 OOS OOti 00£ OOZ OOT 0 0 0 0 0 0 N r-1 r-I f V (4n9N-1aa3) uoLIena13 O 2 a o r o I 1 , • •1 1 /� • � p O t � U � UO G ~ ~ I /• L N li t f] 2O Y G x Y - If ' 1 1, • Y a _I a c o N o 1 . N O E 2 N £ R A • Z Q Z Q Z O Z 1 1 / 1� 1 7/1 11 1 1 1 •I/ � 1 1 1 1 1 , 1 1 1 1 � � � 1 1 1 1 ' I I I � 1 1 1 ' 1 1 1 1 1 1 � � � 1 1 1 � = I 3 ..... ...g. .g........... 1n 0 Ln 0 Ln 0 Ln r1 (dn9N-100j) uo •en013 Figure A-34: Measured beach profiles at baseline Station 073+39, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 008 OSL OOL OS9 009 OSS OSti CO E OOti o L 0 00£ r_ 4- 0 OSZ OOZ OST OOT OS 0 July 2018 A-35 olsen associates, inc. oo-V'z OOE'z OOz'z 00 000'z 006'T 008'T OOL'T 009'T v OOS'T v OOti'T •v In ru 00£'T CO E OOZ'T 41 OOT'T 41 000'T 0 006 N 008 0 OOL 009 OOS OOti 00£ OOZ OOT 0 0 0 0 0 0 fV r-1 ri fV (4n9N-1aa3) uoLIena13 � I 0 Y U U , N N 0 L U , a O a N O d 1 I W O O! ti W N � Ol 00 E E O > N ZaZaZO�Z� 'I I 1'Ii• 1 /1� 1 I • 1 1 1 1/ � I / I/' • � 1 / 1 1 1 f I 1 � I I � 1 1 1 1 � � � � � 1 1 1 1 1 1 1 1 1 1 1 1n 0 1n 0 Ln 0 Ln (dn9N-100j) uo •en013 Figure A-35: Measured beach profiles at baseline Station 076+37, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 008 OSL OOL OS9 009 OSS OSti CO E OOti o OSE 41 0 OSZ OOZ OST OOT OS 0 July 2018 A-36 olsen associates, inc. 0 0 0 0 0 fV r-1 ri N (4n9N-1aa3) uoLIena13 oo-V'z 00£'z OOZ'z OOT'z 000'z 006'T 008'T OOL'T 009'T v OOSIT v OOti'T •v In 00£'T m E OOZ'T o v OOT'T �_ 000'T 0 v 0 006 N 008 0 OOL 009 OOS OOti 00£ OOZ J OOT 0 1 � 1 I 0 0 ' o s N O N d '/� O N ti N •"� N "� NO '-I � N M 1 /•/ 1 4 1, 1 N O N W N 00 a Y a a C a ti N E E E O T j T 1 Z Q Z Q 2 O Z 1 /' �♦ I I♦ I I I I I ' 1 1 , '1 I I 1 ♦1 / 1 I • II ` 1 1 / /r 1 rl •� 1 1 I' 1 1 ' ♦r ,I • 90000 1 1 1 I 1 � � � 1 1 1 1 1 � � 1 = 1 3 2 2 Ln 0 u1 0 1.n 0 Ln (dn9N-100j) uo •en013 Figure A-36: Measured beach profiles at baseline Station 084+16, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) Os8 008 OSL OOL OS9 v OSS - OOS CO E OSti o 00V 0 0 OS£ 0 00£ OSZ OOZ OST OOT OS July 2018 A-37 olsen associates, inc. 1 , oo-V'z 1 1 m I oo£'z N 1 I ►. m 00 1 OOZ'z N w 00 1 I ► m O 1 OOT'z I Q 1 I 000'z I ^ 1 1 1 I 006'T 1 I � 008'T I I � � OOL'T I I � 009'T 1 OOS'T v 1 1 I I I v OOti'T v N 00£'T CO 1 1 1 1 I OOZ'T o 1 1 I I I U OOT'T ru 1 1 1 4� to 1 1 000'T I I I 1 0 006 1 I • I , 008 0 1 1 1 � ► OOL 009 1 I �1 OOS 1 , 1 , 1� ' l 00ti ( u W 00£ � 00Z 0 OOT N 0 O v��i 0 1 , • o _ 3 U • Y i/ ► � O i+ O C � � � � i 1 ,• , I �n lu7 l9 0 N- D 1 O o u o `o d° o r a L Y Y Y N 6 lr m>= o>;> z ¢ z ¢ z O z ' / / � 1 1 1 1 '• 1 ►' /I, 1 I, I � I � � � I I I ► � 1 1 � � � � � 1 ._. 1 ... 1 1 1 1 ... .. ... 3.. 0 0 0 0 0 1n 0 L n 0 1n 0 Ln (V r-1 ri N r-1 r-1 r I r I (4n9N-1aa3) uoLTena13 (dn9N-1aaj) uo •ena13 Figure A-37: Measured beach profiles at baseline Station 088+23, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 008 OSL OOL OS9 009 OSS OSti CO E OOti o OS£ In OSZ OOZ OST OOT Os 0 July 2018 A-38 olsen associates, inc. 1 oo-V'z 1 1 Ln I OO£'z 1 I + � N I OOZ'z N p1 m O 1 OOT'z I Q 1 I F- 000'z I ^ 1 1 006T I 1 I � 008'T I r l OOL'T ........... I � ' 009'T ' I v OOS'T 1 I I v OOti'T v N 00£'T CO 1 1 1 1 I OOZ'T o 1 1 1 I I U OOT'T 1 1 I � 1 I 000'T 1 � ' ' I 1 O 006 I ' I I 4- 008 001 ' ' I 009 ' 1 OOS = OOti W 00£ ! CO 1 I 2 OOZ c 1 I I � 0 OOT N 0 1 O 1 1 1 0 � ri « � vf0i vf0i a O NO F L O 1 •/ •-I W N W Y G S y N 1 1 /\ � / O 1 N •-I N � NO 'O-I � N M I I 1 /� I 0�0 N E E E Z Q Z Q 2 O Z 1 1 , 1 I 1 1 I !I 1 / 1 I 1 / 1 1 1 1 I I I I 1 1 1 1 � I I I I 1 i I � = 1 I 3 0 0 0 0 0 Ln 0 Ln 0 Ln 0 Ln (4n9N-1aa3) uoLIena13 (dn9N-1aaj) uo •ena13 Figure A-38: Measured beach profiles at baseline Station 092+15, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) Os8 008 OSL OOL OS9 v OSS - OOS CO E OSti o OOti Ln in N OS£ 4- 0 00£ OSZ OOZ OST OOT OS July 2018 A-39 olsen associates, inc. 0 0 0 0 0 (V r-1 r-1 N (4n9N-1aa3) uoLIena13 oo-V'z oo£'z o ` . .. U o 0 a o0 1 / 1 TT 77 , L OO o Y •-I O NO F •; L O 1 N O N i Y N 1 / I 1 1 , 000'(,77 a a c a o o= 0 1 1 , t I, 006'T 01 O N W N n N 00 a Y a a a •-I N O / W J W N a W o 008'T Z Q Z Q Z O OOL'T I 1 1 / 009 T 1 1 OOS'T v 010ti'1 00£'T m 1 ;J' / E / ' 1 /0 OOZ'T OOT'T I , 1 O 006 I # / 1 N I 008 O 1 r I ' 1 • OOL III 009 , I 1 N 1 I 1 1 OOS P I ; OOti I i I 1 1 1 00£ t, 1 1 �r � � 1 1 ' OOZ 1 OOT 0 1n 0 L n 0 Ln 0 r-1 (dn9N-100j) uo •en013 Ln r-I Figure A-39: Measured beach profiles at baseline Station 097+10, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) Oss 008 OSL OOL OS9 IIIj:� v OSS - OOS CO E OSti o OOti 1 0S£ O 00£ OSZ OOZ OSZ OOZ OS July 2018 A-40 olsen associates, inc. OOVZ I 1 1 00 I � 00£'Z O1 I �p N I OOZ'Z N O 1 OOT'Z I 1 I F— 000'Z I ^ 1 1 006'T I 1 I 008'T I I I I OOL'T I I 009'T .-. ' 1 I v OOS'T 1 I r v OOti'T v V) ru 00£'TCO 1 1 00Z'T 1 1 U OOT'T 1 I i 1 I 4� 1 I t 000'T 1 I I O 006 N ' ' 0 008 1 1 OOL 1 I� 009 1 ' h 00S = V -y ' w 00£ ' I I m I = OOZ I r ' ... . 1. I. . . � 'O, OOT 0 1 O i 1 1 O O C 3 � a� a� •• g u o v o a o "s o 1 o 2 N O N L L 1 O d N 0 N •-I ry '-I O lD 0�p N f.0'1 ` I y O E W W N N O Z Q Z Q 2 O i Z i 1 a it 1 ' 11 • 1 � � � � �• 1 1 •1, r, I I p I I ` , I 11 1 I 1,, I 1 n . I , I •' / 1 I 1 1 � ' I 1 • 1I I r 1 I I I � � ' I 1 1 0 0 0 0 0 1n 0 L n 0 1n 0 Ln (V r-1 ri N r-1 ri I r I (4n9N-1aa3) uoLIena13 (dn9N-1aaj) uo 'ena13 Figure A-40: Measured beach profiles at baseline Station 102+08, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 006 058 008 OSL OOL v 009 _ OSS CO E 005 0 Ost 00ti CZ 4- 0 OS£ 00£ osz ON OST OOT July 2018 A-41 olsen associates, inc. oo-V'z 00£'z OOz'z OOT'z 000'z 006'T 0o8'T OOL'T 009'T v OOS'T v OOti'Tru •v 00£'T CO OOz'T o 41 OOT'T LA 000'T 0 0 006 N oos 0 OOL 009 OOS OOti 00£ 00z • OOT 0 0 0 0 0 0 (V r-1 r-1 N (4n9N-1aa3) uoLIena13 o I o r o � � ♦y _ a !0 o n 0 0 u0 m~ a~ t ' / /♦ o Y o .ti o o a 0 a° a o C 000 / E E N E 0 E N ' Z Q Z Q 2 O Z 2 ♦ ♦/ I � � � � � � Ir ♦I I n ,l• � 41 •X X dW ' .♦ to I r, 9 = 3 1n 0 L n 0 Ln 0 Ln r-1 (dn9N-100j) uo •en013 Figure A-41: Measured beach profiles at baseline Station 106+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 006 058 008 OSL OOL v 009 - OSS CO C 005 0 OSV 41 0 OS£ 00£ OSz ON OST OOT July 2018 A-42 olsen associates, inc. I 1 1 I O' 1 ► 1 O1 I + 1 CO I N O 1 1 I 1 1 I 1 I 1 ' I I I ^ 1 v, 1 1 1 1 4 I I I I I I I I I I I I I ' I 1 ' 1 I I I 1 1 1 I I I 1 1 I I 1 1 1 I I I 1 1 1 1 I 1 I 1 I I I I I I 1 1 1' 1/ • I 'I • 2 u a WI co 1,a. '' I I F- I I I I I I 0 0 0 0 0 (V r-1 r-1 N (4n9N-1aa3) uoLIena13 oo-V'z 00£'z OOZ'z 00 000'Z 006'T 008'T OOL'T 009'T v OOS'T U- v OOV'T •v In ra 00£'T CO OOZ'T v OOT'T 000'T v 006 N 008 0 OOL 009 OOS OOti 00£ 00 • s;,l OOT 0 1 , O 1 1 OC L U •`+ 1 0 6 0 o. o. O d ' .I 0 a 0 O O ♦? H N li 1 / , •-I Q u, '. L '• C � C Y V d O d N H �� I ► N •-I N "� N� '-I � N M I ► 00 a Y E a p E N N > O � i Z Q Z Q 2 O Z it ; a �► I 1 , I, ,1 1 I � I I I I 1 1 1 I I � I I I I I I 1 I 3 I � I ol I I I I = 1n 0 L n 0 Ln 0 Ln r-1 (dn9N-100j) uo •en013 Figure A-42: Measured beach profiles at baseline Station 110+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 006 OS8 008 OSL OOL v 009 - OSS CO E 005 0 OSti 0 OS£ 00£ OSZ 00Z OST OOT July 2018 A-43 olsen associates, inc. OOS'z OOti'Z 00£'z OOZ'Z OOT'Z 000'z 006'T 008'T OOL'T v 009'T v OOS'T v In OOt7'T m E 00£'T v OOZ'T OOT'T L 000T N 4- 006 0 008 OOL 009 OOS OOti 008 00Z OOT 0 0 0 0 0 N r-1 r-I f V (4n9N-1aa3) uoLIena13 1 1 , I • I p 0 1 _ 0 4tV a 0 0 ` .. g o . 0 u o v a~ 1 ./ o n 0 o 0 0 , m~ t. t o .ti o N O N Y o f � a o a0 O d N H 1 •/ , O O N O N � O N - O - �. N O E E N E° .M.. 0 0 0 009 0 - 0 O T 0 Z Q Z Q 2 O Z 1 1 1 •� 1 � 1 11 1 1 5• u � � ■I4 1 , , II 1 1 1 1 1 f 1 1 1 1 1 1 1 1 1 1 I 1 I I 1 � I I r � ' � = I 3 1n 0 1n 0 Ln 0 Ln r1 (dn9N-100j) uo •en013 Figure A-43: Measured beach profiles at baseline Station 114+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 006 OSV 008 OSL OOL v 009 - OSS CO E 005 0 OSti 41 0 OS£ July 2018 A-44 olsen associates, inc. 1 1 I I O' 1 I O1 I 1 I O1 fM r--i 1 I I 1 I 1 I 1 I ^ 1 1 1 1 I I I I I I I I I I I k• I I I f I I I I I I I I I 1 1 1 1 1 1 1 1 1 1 I I I 1 1 1 I I I 1 I I I I I I I I I / 1 1 too 1 1 1 ; I• ,o 1 Q W N m I � 1 � I O N 0 0 0 0 0 (V r-1 ri N (4n9N-1aa3) uoLIeAa13 OOS'z OOti'Z 00E'z OOz'z OOT'Z 000'Z 006'T 008'T OOL'T v 009'T v OOS'T v OOVT m E 00£'T v OOZ'T OOT'T v 000'T N 4- 006 0 008 OOL 009 OOS OOti 00E OOZ OOT 2 C I f'I ; yt�„ 0 0 0 00 L 2 V 2 I ,o Y+ c c �I I A 0:G 6 i+ U C U I / / 0 O. 0 O O H tl H L I I Q Y V u a. O O N 0 Y d C d N� N�� ti� 1 •, •� , , N e-I N � N ti � N M I , ' 0 0 `y O W � N N 1� N 00 I • // E N o z° a' z° a z° z° / 1 ' b ,I � 1 Ip I i IT 1 � I I i I I I I I I I I I I I I r I 1 � ► � I ...� 1 I .......... 1n 0 L n 0 Ln 0 Ln r-1 (dn9N-100j) uo •en013 Figure A-44: Measured beach profiles at baseline Station 118+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 006 OS8 008 OSL OOL v 009 - OSS CO E 005 0 OSV 0 OOti C 4- 4- 0 OS£ 00£ OSZ ON OST OOT July 2018 A-45 olsen associates, inc. 1 1 i I I 1 O1 I , I O1 I I 1 I � N M (V 1 1 I I 1 1 I 1 I 1 I ^ 1 1 1 1 I I I I I I I I I I I I I I I 1 I I I I I I I I 1 1 1 1 1 1 1 1 1 1 1 I I 1 1 1 I I I l 1 1 1 I I c lit 1 I I I I 1 I I 1 1 •: 1 I 1♦ ♦ 1 1 1 1,♦ / ' ♦1 ,1 1 ` 1♦ , 1 I" • A � Q W 1 1 1 1 1 / I D I• I I `w O O O O O (V r-1 ri N (4n9N-1aa3) uoLIena13 oo-V'z 00£'z OOZ'z 00 000'z 006'T 008'T OOL'T 009'T v OOS'T v OOti'T •v 00£'T m E 00Z'T v OOT'T 4-1 000'T 0 006 N 4— 008 0 OOL 009 00S 00ti 00£ 00Z OOT 0 1 '♦ 'r 3 1 ' ♦. r �o=0 -- t2 CO L U Y O. Y+ C '7 1 /to H vf0i U a+ • / v O N s p = L O L 1 / ♦ I O. O. C � p O � O 1 1 1♦ � , o� ti� N��� O d N £ N 1 I � 1 I ♦ j > - > •/, Z Q Z Q Z O Z 1 I , I / 1 I I 1♦I 1♦ 1 4. 1 . ' r I �� r ♦ I I J I I ' 1 1 I 1 I I � � I /1 ♦ I I I � I 1 . g �........... r-1 (dn9N-100j) uo •en013 Figure A-45: Measured beach profiles at baseline Station 122+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 006 058 008 OSL OOL v 009 — OSS CO E 005 0 OSti 41 0 0 OOti 0 OS£ 00£ OSZ ON OST OOT July 2018 A-46 olsen associates, inc. oo-V'z oo£'z OOz'z OOT'z 000'z 006'T 008'T OOL'T 009'T v OOS'T v OOti'T •v V) 00£'T m E OOZ'T v U OOT'T 41 000'T 0 006 N 4- 008 0 OOL 009 OOS 00ti 00£ 00Z OOT 0 0 0 0 0 0 (V r-1 r-1 N (4n9N-1aa3) uoLIena13 I , ,• , / O �+ C a+ ,-. 0 I a 5 o 0 10 V I I ./ /s• 2 EVEN v o No W — p ? T z o i I.1 zo II ' , I I , k III l •I � I / 1 • I 1 / 1 I/1 1 I{1 / 1II II , M ♦ 1 I I •, / 1 1 /1 I 1 I I II / 1 1 1 I I 1 I / 1 I 1 1 I I 1 / I 1 1 • 1 I 1 I I I I I 1 I 1 I I I I 1 1 I 1 1 1 = 3 1n 0 1n 0 Ln 0 Ln r-1 (dn9N-100j) uo •en013 Figure A-46: Measured beach profiles at baseline Station 126+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) Os8 008 OSL OOL OS9 v OSS - OOS CO E OSti o OOti 1 0 OS£ 0 00£ OSZ OOZ OST OOT OS July 2018 A-47 olsen associates, inc. oo-V'z OOE'z OOZ'z OOT'z 000'z 006'T 008'T OOL'T 009'T v OOS'T v oo-V'T In ru OOE'T CO E OOz'T v OOT'T 000'T v 0 006 N 4- 008 0 OOL 009 00S 00ti 00£ 00Z OOT 0 O O O O O (V r-1 r-1 N (4n9N-1aa3) uoLIena13 4 I , � / II 1 I I 1 1'1 1 I,r I 1 r 1 , 1 / I I II 1 1 1 •� I , I I I / 1 I 1 1 1 1 / 1 / 1 1 0 I I I I _ � w u •�% I 1« 1 ..• N O •' N •' II .... O N ON n � E E N E °1 N E H • • • / • + 1 i o z° ¢' o ¢ o zo zz i I I ' I I I I I 1 1• � IIII Ln O u1 O Ill O Ln (dn9N-100j) uo •en013 1 I Figure A-47: Measured beach profiles at baseline Station 130+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 008 OSL OOL OS9 009 OSS Ost CO 00-V OS8 0 0 008 0 OSZ OOZ 0S V OOT OS 0 July 2018 A-48 olsen associates, inc. 1 1 1 I 0 ' 1 1 0 1 I + 1 M I rn 1 1 I 1 1 I 1 I 1 1 1 I 1 1 1 1 I ( . / I I I I I I I I I I 1 I I I ... ... 1 ... I 1 1 1 I I I 1 1 I I 1 1 I I 1 1 1 I I I 1 1 1 I 1 I 1 I I I I I 1 1 1 A01 1 1 1 1 1 1 1 , 1� ,1 1q ' I� I •1 , A 1 r , r I ' I I I I I � I I I I I I• I 0 0 0 0 0 (V r-1 r-1 N (4n9N-1aa3) uoLIena13 oo-V'z oo£'z OOZ'Z OOT'Z 000'z 006,T 008'T OOL'T 009'T v OOS'T v OOVT v 00£'l O 00Z'T v OOT'T 4-1 000T v L 0 006 N 4- 008 0 OOL 009 00S 00ti 00£ OOZ OOT 0 I 1 I 1 •, , ► I I 1 •, ' / I I , 1 , I � I 1 • f' �i I� r 1 , I I I 1 I 'C J / 1 I 1 1 1 I ' I I I I I I I I I I I I I I O m i, N U O y ti U• N 6. I 1 I N' � u1 h w V• V• O o N U O L o I 1 1 O rO, E N a+ O Y • • • • I .+r I nO, Z Q Z Q Z O Z I I ' 1n 0 1n 0 Ln 0 Ln (dn9N-100j) uo •en013 1 Figure A-48: Measured beach profiles at baseline Station 134+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 008 OSL OOL OS9 009 OSS Ost CO E OOti o L 0 00£ r_ 4- 4- 0 Osz OOZ OST OOT OS 0 July 2018 A-49 olsen associates, inc. El 0 0 0 0 0 (V r-1 r-1 fV (4n9N-1aa3) uoLIena13 OOti'Z 0 00£'Z 2— '• •I / OOZ'Z �a��y� '• �/ OOT'Z 0 N - I / o o o 6 OOOZ 006'T E U E N E > z ¢' z a z o� z� �• 1� 008'l I I I ) I OO/-T 009'T 1 OOS'T v • 00£'l; m E OOZ'T • ' i v OOT'T f 000'T 0 ' 006 i• / (1/ O 008 i OL OOL 'I 1' ✓ I 009 i OOS OOti r I ' 1 00£ ' OOZ ► ' OOT = 3 ...�. � .......... � 0 1n 0 L n 0 Ln 0 r-1 (dn9N-100j) uo •en013 Ln r-I Figure A-49: Measured beach profiles at baseline Station 138+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) OS8 008 OSL OOL OS9 1910� v OSS - OOS CO E OSti o OOV 41 0 OS£ r- 0 00£ OSZ OOZ OSZ OOZ OS July 2018 A-50 olsen associates, inc. 1 1 I I O' 1 1 O1 I + ' ro 1 ' I 1 1 I 1 I 1 I I ^ 1 1 I I , 1 1 I I I I I I I I I I 1 I ' 1 1 1 1 1 I I 1 1 1 I I I 1 1 1 I 1 1 1 I I I 1 1 1 I I I 1 1 Jr / I 1 , 1 1 , 1 1 • I. I 1� 1 t I ' Q W 1 � I I � � O 0 0 0 0 0 (V r-1 r-1 fV (4n9N-1aa3) uoLIena13 ' OOtiZ / 1 N / 00£'Z o-0 ,;� OOZ'Z a a a- OOT'Z C g4 oo�oa� OOO'1.7 N O N Ul � 006'T v v' v- o a z ¢' z a 008'T 009'T • / 1 ,1 OOS'T v OOti'T ' 00£'l O OOZ'T r (U U � ' OOT'T O ♦1 006 N 008 0 1 / � 1 OOL i '� {/ .I 009 1 � OOS ' .yr 1 I 1 � OOti . 1 00£ 1 1 � 1 1 OOZ , 1 1 1 OOT .. ... .... ... ... _• 3 0 1n 0 L n 0 Ln 0 Ln r-1 (dn9N-100j) uo •en013 Figure A-50: Measured beach profiles at baseline Station 142+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) OS8 008 OSL OOL OS9 v OSS - v c OOS CO E OSti o 00V OS£ 4- 0 00£ OSZ OOZ OSZ OOZ OS July 2018 A-51 olsen associates, inc. 0 0 0 0 0 (V r-1 r-1 fV (4n9N-1aa3) uoLIena13 oo-V'z oo£'z OOZ'z OOT'z 000'z 006'T 008'T OOL'T 009'T v OOS'T v OOti'T •v In 00£'T m E OOZ'T v U OOT'T N 000'T 0 v 0 006 N 008 0 OOL 009 OOS OOti 00£ 14 OOZ OOT 0 o �• 0 0 -F 3 v O. 1 i c N o r Y '0'o � u d c d 1 V • L L � � � O ' 1 I / Y •+ V d Y 1 1 1 CO N CO 1 I 1 o H E N E L N � O T T / I z o z i z a' z a I I I 1 1 1 'h II II 1 1/ 1 ♦ ♦ I 1 / 1� /1 I 1 I 1 � 1 • I' r ►' 1 1 1 1 I ' I I 1 I I � I 1 � I � � 1 .. ... 1 ' 1 ... 1 ' 1 1 �.� ... ... 1n 0 L n 0 Ln 0 Ln r-4 (dn9N-100j) uo •en013 Figure A-51: Measured beach profiles at baseline Station 146+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) Os8 008 OSL OOL OS9 v OSS - OOS CO E OSti o OOti 00£ OSZ OOZ OST OOT OS July 2018 A-52 olsen associates, inc. oo-V'z oo£'z OOZ'z OOT'z 000'z 006'T 008'T OOL'T 009'T v OOS'T v OOti'T •v In ru 00£'T CO OOZ'T v OOT'T 000'T 0 006 N 008 0 OOL 009 00S OOti 00£ OOZ OOT 0 0 0 0 0 0 (V r-1 ri N (4n9N-1aa3) uoLIena13 1 1 /w i ► i 2 1 0V 0 C J U 3 1 ti N a m O O 1 o o 0 0 U j I `N a ° tl i+ 1 C C O N O O N N N N M E " E N E a N E N O 1 1\ 1 I Z Q Z Q Z O Z 2 ' / 1 ► 1 1 1 , ' I I ►I 1 \� � I 1 / I 1 I4 I 1 �I /1 1 � I I � III 1 ► • I) 1 � 1 I so 1 1 ► 1 � � � � 1 1 I I I / ► 1 / � � � � � I 1 1 1 / 1 / � � 1 1 1n 0 1n 0 Ln 0 Ln (dn9N-100j) uo •en013 Figure A-52: Measured beach profiles at baseline Station 150+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) Os8 008 OSL OOL OS9 v OSS - OOS CO E OSti o OOti 41 0 OS£ r- 0 00£ OSZ OOZ OST OOT OS July 2018 A-53 olsen associates, inc. OOS'z OOti'Z 00£'z OOZ'z 00 000'Z 0061T 008'T OOL'T v 009'T v OOS'T v OOt7'T m E 00£'l; v OOZ'T 41 Ln OOT'T 0 000T N 4- 006 0 008 OOL 009 OOS OOti 00E OOZ 002 0 0 0 0 0 (V r-1 ri N (4n9N-1aa3) uoLIena13 1 ? o o - C - o y OR. H io « o .~', o 1 1 / 01 1° c. o« u c a u I x ti 0 ry u .~'. r o In u S d N O N 'O O 1 o N d N O N o 2 ry G i oo O mo M Ooj g p >. . p I I Z Q Z Q Z O Z + 1 I' I �► 1 1 1 1 q1 , 1 /1 1 y 1 ■7 / 1 1 A 1 1 1 1 ' � 1 1 1 1 1 I 7� ► 1 I 1 1 I I = 3 L i Ln 0 Ln 0 Ln 0 Ln (dn9N-100j) uo •en013 1 1 Figure A-53: Measured beach profiles at baseline Station 154+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 006 058 008 OSL OOL v 009 - c OSS CO E 005 0 OSti 41 0 OOti 0 OS£ 00£ OSZ OOZ OST OOT July 2018 A-54 olsen associates, inc. 0 0 0 0 0 (V r-1 ri N (4n9N-1aa3) UoLIena13 OOS'z 1 OOti'Z / O O _ - - 00£'Z _ _�3y�Y /► O Y (7 1 O ie O O U U , OOZ'z oLn a o s o j 1 O a OOT'Z d N d C OOO'Z O O fV V G a a a N �00 CD a I O w o 0 a N > N , . J 006T N N� z° a' z° a z° o z° , 008'T OOL'T I l l i ICI 009'T OOS'T v II OOti'T m E1 ., 00£'T I I� OOZ'T � f% OOT'T 000'T N 1 006 0 �i � I 008//' 001 J 009 / ' 1 , OOS y � I 00-V oo£ I ; OOZ I ' .. J.. _. 3 .......... OOT 1n 0 1n 0 Ln 0 r-1 (dn9N-100j) Uo •en013 Ln r-I Figure A-54: Measured beach profiles at baseline Station 158+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 006 OS8 008 OSL OOL v 009 - v c OSS CO E 005 0 OSV 0 00-V c- 4- 0 OS£ July 2018 A-55 olsen associates, inc. I I I 1 I 0 I 0 1 + N I 1 I,�VI 1 I I 1 Q 1 I I I ^ 1 1 I ( I 1 1 I I I I I yl I I I 1 I I I 1 1 I 1 1 1 I 1 I 1 I 1 I 1 I 1 I I 1 I 1 I 1 1 I 1 I / 1 I 1 I 1 I I I I I I I I I 1 1 I 1 1 1 I , 1 1 1 1 AV 1 I 1 I 1 r 1 2 ' V W CO I I I I I I �0 � I oo-V'z os8 1 oo£'z 0008 _0 I OOZ'Z a •, OOT'Z s aoo��ri� 1 OS/ - 000'Z CD O fV N O Y > t S p. d 1 • 1 f L p p 2 20 OOL 006'1 oo� CD .N4 CR21 E o N a o 0 N N ' • 008'l zazazo z If OS9 OOL T 1 ' 009 009'T OOS'T v Oss v v I 1 1 v OOti'T v ru 00£'T it I (U OOS N m /I I If 00Z O T f , U o OSti , , �i OOT'T ru 00V In 000'T L% 1 f • 1 006 N OS£ Ln 0 1 1 1 4- 0 008 y 1 00£ OOL I • � I 1 009 OSZ 1 1 I OOS OOZ I OOtir I 00 I I OSi 00Z I I I 1 I I 00 T L OOT 1 _. 1 3........... .. w .. 0 OS 0 0 0 0 0 1n 0 L n 0 1n 0 Ln (V r-1 ri N r-1 (4n9N-1aa3) uoLIena13 (dn9N-1aaj) uo •ena13 Figure A-55: Measured beach profiles at baseline Station 162+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) July 2018 A-56 olsen associates, inc. I 1 1 I 0 ' 1 1 0 1 I (V 1Z 1 I 1 I I I I ^ 1 v , 1 1 1 1 ► I ► I ► I ► I I I I I I I I I ' I I I I I 1 1 1 I 1 I 1 1 1 1 I I I ► 1 1 I I I 1 1 1 I I 1 ► 1 1 1 1 I I I ► I 1 I I 1 I I I I 1 I J 1 1 1 I 1 1 / 1 1 1 I ' 1 1 1 I I I 1 1 � 1 1 2 ' V ' a WM I W 1 I I I I ► 1 I O hj 'w O O O O O (V r-1 r-1 N (4n9N-1aa3) uoLIena13 OOVZ OOCZ OOZ,Z OOT Z 000 z 006'T 008'T OOL'T 009'T OOSIT v OOVT •v In 00£�T m E OOZT 4, OOVT �_ OOO'T v L 006 N 008 0 OOL 009 OOS OOti 00£ 00Z OOT 0 1 a , O } O N h O Y C F' C ' 1 • '/ c vOf m C ., V1 V u = 1 o no �La aa O � � S �• 2 L �. L , rI I c a o 1 1/ cD E E E , z Q z Q z 0 z II /► I i' � '�► I I I I 1 I 1 I I I I I I I � ,• I 1 I 1 , 1 I 1 / I 1 / I In 1,► I 1 1 • 1 � / 1 / 1 �, 1 • 1 1 I I 1 1 1 1 �� / ► ► 1 1 1 1 1 1 I I 1 1 1 ' 1 1 1 . . . + .. . . . . . Ln O u'1 O 1.n O Ln (dn9N-100j) uo •en013 Figure A-56: Measured beach profiles at baseline Station 166+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 008 OSL OOL OS9 009 OSS OSti CO E OOti o OS£ 41 0 OSZ OOZ OST OOT OS 0 July 2018 A-57 olsen associates, inc. I 1 1 I 0 ' 1 1 0 1 I +ro ' O 1 1 I I I \ 1 1 1 I I 1 1 I r ^ 1 1 I I 1 1 I r I I I I / I I I I � I! I I I . .I i 1 I r 1 I 1 I 1 I 1 I I 1 I 1 ' I 1 I I 1 I 1 1 1 I 1 I I 1 1 1 I I I I I I I I 1 1 I 1 1 1 1 1 I ' 1 I 1 1 I ' 1 , 1 1/ • 1 I ' V 1 r Q WM I 1 W I I I O I � I N J� I 0 0 0 0 0 N r-1 r-I f V (4n9N-1aa3) uoLIena13 oo-V'z 1 oo£'z CI a. 1 O } O , OOZ'Z C'. U U 1 0OT z o fl- o 0 0 ( a. L 0 0 0' Z 0r NO CD le a N a d N. O o O o g a .. / 006'T o . CDCD N E E a N E'. N N V N N 01 008l - O zQzQz0�z� / 1 , OOL'T 1 1 , 009'T v I 1 I►' OOS'T v 1 11 I V) 00£'T m 0 .I,o OOz'l o r . OOT'T 1 1/ 000'T 006 / a 0 008 1 , 1 OOL 1 i 009 r' 1 1 OOS 1 1 OOti1 1 001 00£ I 1 1 00Z I I I 1 ' 1 1 OOZ I 1 0 1n 0 1rn 0 Ln 0 r-1 (dn9N-100j) uo •en013 Ln r-I Figure A-57: Measured beach profiles at baseline Station 170+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 008 OSL OOL OS9 009 OSS OSti CO E 00-V OS£ 1 00£ r_ 4- 4- 0 OSZ OOZ OST OOZ OS 0 July 2018 A-58 olsen associates, inc. I 1 1 I 0 ' 1 1 0 1 I + ' 1 1 I I 1 1 1 I I I ^ 1 1 I I 1 I I I I I I I I I I I I { f I I I 1 1 1 1 I I 1 I 1 I 1 I 1 I 1 I I 1 I I 1 I 1 1 1 I I 1 I 1 I I 1 I I I I I I I I 1 1 I 1 1 1 1 1 / 1 1 1 1 1 1 1 � I II 1 1 2 ' V ' a m I I D ♦� � I I 0 0 0 0 0 0 (V r-1 ri N (4n9N-1aa3) UoLIena13 oo-V'z oo£'z o: o 7 H H fl 3 N O U U a 00T'z o 8 0 0 � ri CD •= S p�. d 1 ' 000z NO~a 0 C Y d Ni• I � I d CD yNS d ID C ID g 0 1 1 006'T I v o o a`i '^ a`i C'3 n CR 2 a W I a N V � � N o N E c c ' 008'T z¢ z¢ z O z OOL'T 009'T � I 1 OOS'T v v OOti'T I 1 I 1 i, vI 1 00£'T CO E ♦1 1 `I ' OOZ'T U � 1 / OOT'T r 1 \ 4. 000'T I , 006 N � 1 1 008 0 1 I ' 1 I . / OOL ,y 009 1 OOS 1 OOtiI � / I 1 1 I oo£ ' I � 01DzI I ' 1 OOT ' = 3 .. ... �........... 0 u1 0 1n 0 1n 0 (dn9N-100j) Uo •en013 Ln c-I Figure A-58: Measured beach profiles at baseline Station 174+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 008 OSL OOL OS9 009 OSS Ost CO E OOti o OS£ 1 OSZ OOZ OST OOT os 0 July 2018 A-59 olsen associates, inc. 1 1 I I O' 1 I O1 I + 1 I L 1 1 I I 1 1 I 1 I 1 I I I ^ 1 1 1 1 • I I I I I I I I I I 1 I I I 1 1 I I 1 1 1 I I I 1 1 1 I I I 1 1 I I 1 1 1 I I I 1 1 1 I I 1 1 1 1 1 ► I I 1 1 1 1 ► / 1 1 1 1 1 1 1 1 I 1 1 1 1 I A. , ' � l ' V ' m I I I I I I I �� I I .0. cn O 0 0 0 0 (V r-1 r-1 N (4n9N-1aa3) uoLIena13 OOE'z OOz'Z OOT'Z 000'Z 006'T 008'T OOL'T 009'T OOS'T v OOVT v 00£'T v In OOZ'T m E OOT'T v U 000'T 4-1 to 006 v L 0 008 N OOL 0 009 OOS OOti 00E C ooz ooi 0 OOT 1 o y o o 0 ` U U c'7 H I 1 o fl o 0 o A "' o S O� d 1 I N O N C) i N O Y Y j 9 L ' , ► .�... cD a+ .�... N C o �. .d_. CO Ni O � 2 mo N �, FR M 1 ' I 2 O G ' o a N E N z Q z Q o z O z'. I ' 1 , 1 I , 1 I 1 , I I I 1 • , I I 1 I I 11 I I 1 / / 1 1 / 1 ✓ /✓1 1 � 1 1 � 1 1 1 / 1 1 ��1 1 1 1 1 ,• 1 / I 1 1 1 1 ► I I 1 1 ► I 1 I I I 1 1 1 1 1 1 1 11• 3 3 - C= L CJC L Ln O ul 0 Ln O Ln (dn9N-100j) uo •en013 Figure A-59: Measured beach profiles at baseline Station 178+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) OSL OOL OS9 009 OSS v OSt7_ 00V CO E OSE o 00E 41 In 0 OOZ OST OOT os 0 Os - July 2018 A-60 olsen associates, inc. 1 1 I I O 1 1 I ' I O1 I + 1 I 1 1 I I 1 1 I 1 I 1 I I I ^ 1 1 1 1 I I I I I I I I I I 1 I I I 1 1 I I 1 1 1 I I I 1 1 1 I I I 1 1 I I 1 1 1 I I I 1 1 1 I I I I / 1 I I I I 1 I 1 / 1 1 1 1 1 1 , 1 1 I 1 1 1 1 1 , 1 1 1 1 1 2 ' a WM W /I I I I •1 � � I I O . 0 0 0 0 0 (V r-1 r-1 N (4n9N-1aa3) UoLIena13 OOE'z OOZ'Z OOT'z 000'z 006T 008T OOL'T 009'T OOS'l; v OOti'T v 00£'T v In OOZ'T m E OOT'1 0 v 000'T 006 v L 008 N OOO L 009 OOS OOti 00E OOZ OOT 0 OOT- o + o V�i n a n o O a d 1 U r - Y 1 N N CD O a CDCD� o CD8 O O � � M , E E oM N E to o I� / zo < z a z o z 1 l 1 I I I 1 1 I 1 , I I 1 1 I 1 I I 1 I 1 I , /r I A 1 ' 'd i I I� I I I / I I/I I At / �' 1 /J I 40. I r I r1 I � I I I I / 1 1 I I 1� I 1 1 1 � � 1 1 1 1 1 1 y 5 � � 1n 0 1n 0 Ln 0 Ln (dn9N-100j) Uo •en013 Figure A-60: Measured beach profiles at baseline Station 182+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) OSL OOL OS9 009 OSS v OSt7_ 00V CO E OSE o OOZ OST OOT IDS 0 OS - July 2018 A-61 olsen associates, inc. 1 1 I I o' 1 o I + 1 1 1 I I 1 1 1 I I 1 ^ 1 1 1 I I I I I I I I I I I I I I I I I I I I I I I I I 1 I I I I I I I I 1 1 I I 1 1 1 I I I 1 1 1 I I I 1 I I I I I I I I I I / I 1 1 1 I I I ► 1 1 I I , 1 1 I e / ► I 1 1 1 I I 1 a m 1 I I — I I I I I O ' w V I 0 0 0 0 0 (V r-1 ri N (4n9N-1aa3) UoLIena13 00-V'z 008'z OOZ'Z OOT'Z 000'Z 006'T 008'T OOL'T 009'T v OOS'T v 0oti'T v In 00£'T m E OOZ'T v OOT'T 000T v L 006 N 4- 008 0 OOL 009 OOS OOti 008 00Z OOT 0 C 1 1 1 ► o + I , , o I cc o 0 4 O CL io O U U , T■ \ O C ~ U Y OCD L ~ � i 0 d 1 NO N O ~ O 1 Op CD ~ CD O N O ~ p CD N O �' O ry0 M I 1 I e > ON e > ~ = t - e > �• xI e i �• I 1 1 e'n I I � I I 1 I 1 01 I � / 1 . 1 1 r/ 1 1 1 1 / 1 � � 1 1 1 1 1 j /' 1 � a IAA 1 ► 1 1 / 1 I ' 1 1 1 I 1 I I 1 � I • fl ► I I I •� 1 I 1 � 3 — Ln 0 1.n 0 Ln 0 1_n r-1 (dn9N-100j) Uo •en013 Figure A-61: Measured beach profiles at baseline Station 186+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 008 OSL OOL OS9 009 Caw Ost CO 00-V OS8 41 0 OSZ OOZ OST OOT Os 0 July 2018 A-62 olsen associates, inc. OOE'z OOZ'Z OOT'z 000'z 006'T 008'i OOL'T 009'T OOS'T v OOti'T v 00£'T v OOZ'T m E OOT'T v 000'T 006 v 0 008 N OOO L 009 OOS OOti 00E OOZ OOT 0 OOT- 0 0 0 0 0 (V r-1 r-1 N (4n9N-1aa3) UoLIena13 1 1/ � ' 3 O O n• ; / n 86 o ad Oe+ I 1 �� � L 1 ~ O d , 1 I r N N O O CDa 1 Y Y N C a ` O I .d.. O O O p a .�-I 2CD o N- N o 1 E " E E E v� , z° < z a z o z I .1 1 1•/ � 1 I lr 9 1 / 1 1 1 1 ' 7 ' ,1 / 1 � 1 / � 1 / � 1 I 1 � � � � � 1 1 1 I 1 1 1 = 3 1n 0 1n 0 Ln 0 Ln (dn9N-100j) Uo •en013 Figure A-62: Measured beach profiles at baseline Station 190+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) OSL OOL OS9 009 OSS slim v OSt7°LL' OOti CO E OSE o 0 OSZ r- 4- O OOZ OST OOT OS 0 OS - July 2018 A-63 olsen associates, inc. 0 0 0 0 0 (V r-1 ri N (4n9N-1aa3) UoLIena13 oo-V'z ' I oo£'z C o 1 � ` ' a O - C u Y O - ' OOZ'z m 0 To �' 4 y u Y l7 c F c ' , OOT'z C o 2 O a 8 8 o O 2�''If O O U U , 1 ' O O H d p d 1 OOO z c-1 c `' N Q a y 0 1 .d.. O O a� O O O ' I 006' 1T CDO CD N CD N p 00 O E E oN E E 008T ' I� 0 ° z e'n < z a z o z , OOL'T I 1 1 ' , 1 009'T v OOS'T ) I ' , I , OOti'T 00£'T CO ;;.I A E o OOZ'T 4-- / ) OOT'T �� I 4J 000'T I , / ) � 0 006 ' 0 008 I • 1/ I 1 001 I I 009 r� OOS OOti 00£ I 1 OOZ ' 3 00< 3 • • • • • `Cj • L CJC • L 0 Ln O Ln 0 Ln (dn9N-100j) Uo •en013 ern r-I Figure A-63: Measured beach profiles at baseline Station 194+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 008 OSL OOL OS9 009 OSS v Ost CO E OOti o OS£ 41 0 0 00£ 0 OSZ OOZ OST OOT OS 0 July 2018 A-64 olsen associates, inc. OOE'z OOz'zz OOT'z 000'z 006'T 008'T OOL'T 009'T OOS'T v OOti'T v 00£'T v In ru OOZ'l O OOT'1 0 41 000'T 41 006 v 008 N OOO L 009 OOS OOti 00E OOZ OOT 0 OOT- 0 0 0 0 0 (V r-1 ri N (4n9N-1aa3) uoLIena13 1 C 1 ' 1 � 0 0 O o f+ C f+ o L i 1 \ / 1 G to a O U O U / 1 o o 0 o c'170 O .. r Y" CDO H d O 1 / N O d � 1 o =CD CD CD C CDw. O O C Q E ° < z a z zo z , 1 � 1 1 � , 1� I / 1 1 I �,Yj , 1 1 1 � , 1 / 1 1 1 1 � � � � 1 1 1 1 1 I I 1 1 1 1 1 = 3 1n 0 L n 0 1n 0 Ln r1 (dn9N-100j) uo •en013 Figure A-64: Measured beach profiles at baseline Station 198+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 008 OSL OOL OS9 009 OSS OSti CO E OOti o 0 S E 0 OSZ OOZ OST OOZ OS 0 July 2018 A-65 olsen associates, inc. I 1 1 I ! O1 O1 I � N Ln O m (V 1 I 1 Q I 1 1 ^ 1 1 1 1 I I I f I I I I I I � I I I I I I I 1 1 I I I I I 1 1 1 1 1 1 1 1 1 1 + 1 1 1 1 1 I 1 1 1 I 1 1 1 1 ` I 1 I I I I 1 I 1 1 1 1 1 1 ' 1 I 1 1 1 1 via 1 1 � 1 1 1 1 Uj CO 1 1 � I 1 I I .0. � � I I III 0 0 0 0 0 (V r-I r-I N (4n9N-1aa3) UoLIena13 oo-V'z c O 1 1 .ryI M OO£'z 3 o t o I t - C - I OOZ'z 0 n .o y io o o I ' OOT'z O o io O n o O O 2 2 O C U a~'• U U } L I I I/ •-I O '� c-1 O Y Q H 0 d O d ' 1 I 1 000'z NONa 006'T CD CD CD CD CD - � = 00 1 E E O N E� ry E ry I I 008'T z° < z a z o z , OOL'T i � • 1: i I I• 009'T i i v OOS'T v '� I I ' OOti'T v I I 00£'T m E1 / OOZ'T v fi 000'T 0 y 1. y 006 p. �1/ 1 /1 008 �1�; / ; OOL , ; + • 1 009 e . ,• I � � 1 1 1 1 OOS 1 ' 1 OOti -' 1 1 1 / I 1 � 1 oo£ � 1 OOZ Of' I � 1 1 DDT .�. = ... ... .+.. 3 ... 0 In 0 L n 0 Ln 0 r-I (dn9N-100j) Uo •en013 Ln r-I Figure A-65: Measured beach profiles at baseline Station 202+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) Os8 008 OSL OOL OS9 v OSS - OOS CO E OSti o OOti 41 0 OS£ r_ 4- 0 00£ OSZ OOZ OST DOT OS July 2018 A-66 olsen associates, inc. 0 0 0 0 0 (V r-1 r-1 N (4n9N-1aa3) UoLIena13 00s'z II OOVZ 1 O O - C - OOCZ —v�i H O. •3 to O a~�+ O 1 I OOZ'z O 0 o O O. 0 CD C U U F? d H , Il�, d d 1 111,1 OOIT 'Z NO d N N i !O Y t d o pd •�-I O O r�-I O •^-I 000'z CD ^ CD CD CD 1 J r— o a o Eo �y 0061 zazaz0 z� , I 008'T 1 1 OOL'l 009'T a) , ' 1 i OOS,T v , OOt7'T m ; I• E o 00£ T �_ o 006 008 OOL 1 � 009 • / OOS 1 � OOti I 1 � 00£ � 1 OOZ ... 1 .�. ... .. .+.. ... = 3 OOT 1n 0 L n 0 1n 0 r-1 (dn9N-100j) Uo •en013 Ln r-I Figure A-66: Measured beach profiles at baseline Station 206+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 006 OS8 008 OSL OOL v 009 - OSS CO E OOS 0 OSti V) 0 OOti 0 OS£ 00£ Osz ON OSZ OOZ July 2018 A-67 olsen associates, inc. 0 0 0 0 0 (V r-1 ri N (4n9N-1aa3) uoLIena13 o0-V'z 00£'z OOZ'z OOT 'Z 000'Z 006'T 008'T OOL'T 009'T v OOS'T v OOti'T •v 00£'T m E OOZ'T v OOT'T 000'T 0 006 N 4- 008 0 OOL 009 OOS OOti 00£ OOZ s OOT 0 1 I O - C O - _ to _ p N �" O t 3 l.7 N O F O 1 1 I I G _ (O G C Y U G U 1 I 0 O C ~ H I O c-1 O Q H d O d 1 I O ` N d y \ a O N O O N o O N G 0 w O O N 1 1 U1 > O > N E 1 z° b0 < z a z o z 1 � 1 � � 1 i 1 � 1 1 •I • I / • 1 I r' j'• ' 1 I I 1 1 1 I I I � = I 3 0 1n 0 L n 0 1n o (V ri (dn9N-100j) uo •en013 Figure A-67: Measured beach profiles at baseline Station 210+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 006 058 008 OSL OOL v 009 - OSS CO E OOS 0 OSti 41 0 OOti c- 0 OS£ 00£ OSZ OOZ OST OOT July 2018 A-68 olsen associates, inc. 0 0 0 0 0 (V r-1 ri N (4n9N-1aa3) UoLIena13 oo-V'z oo£'z 0 3 o 0 C I + OOZ'z O io OCL O � s O .O`• +-' ♦+ U U I ' I OOT'z 9 n 8 O O C I+ O c-1 O 000 z d av O + 006,T CDo CD'+ CDC-D r- m oo � O N O O / 0081 z° ¢' z a z o z , OOL'T 009'T i � 11• OOS'T v 1 N � 1 1 00£'T m E OOZ'T I �' 1 U OOT'T N 000'l; 0 O 006 ' 4— 0 008 r'' �1 1 001 Y. + I r1 o 009 ... .. ... ... ... OOS ' 1 1 OOti� � I I 00£ � � I I OOZ � 1 1 OOT � = I 3 0 1n 0 1n 0 Ln 0 (dn9N-100j) Uo •en013 Ln r-I Figure A-68: Measured beach profiles at baseline Station 214+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 008 OSL OOL OS9 009 OSS OSV M CO E OOti o OS£ 1 OSZ OOZ OST OOT OS 0 July 2018 A-69 olsen associates, inc. 1 , oo-V'z 1 1 0 1 , oo£'z 0 Lf) 1 oo 1 Il OOZ'Z L / 1 I � 1 1 I OOT'z 1 1 1 ' 1 7 000'z ^ 1 1 i 1 I 1 006'T 1 1 t 1 1 0o8'T I I ' 1 OOL'T I 1 , 1 009'T • OOS'T 1 I 1 1 I I 1 / 1 11 1 y I ,I v OOti'T v N 00£'T m E OOZ'T o Qi U 1 1 1 1 1 OOT'Tru 1 1 I Il II. 1 1 I 1 Ul) 000'T L 006 N 1 I ' 1 1 4- 008 1 1 1 , { 1 I OOL 1 1 1 / 1 I , 009 1 ' 1 , OOS 1 1 1 1� 1 , ' w m 00£ 1\ •' _• OOZ 1 1 0 ' w OOT 1 F- 0 J T I I TT I I I I 1 I 1 /1 o - 0 - C - 1 It 3 E V ♦+ N N n V C Y C I °n a n o g u o U U o O c-1 O Q H •E 1 p d I Y /1 .�._ C .�_.. C p .�... O I � ' a CD CD CD i / v fpYf N O N N CD 0 a '' w N r ti E .. E E > e'n > >. z° < z a z o z ` '% 1 I , , � I 'I r I / /Z I � I p I 1 , 1 /I I 1/ 1 , 1 1 1 Of 1 � = I 3 0 0 0 0 0 11, (V r-1 ri N r I (4n9N-1aa3) uoLIena13 0 1n 0 1n 0 Ln (dn9N-100j) uo •en013 Figure A-69: Measured beach profiles at baseline Station 218+00, Bald Head Island, N.C. (Vertical dashed lines indicate physical limits of volume change computations) 008 OS1_ OOL OS9 009 OSS v OOS °LL' OSti CO E OOti o OS£ 1 OSZ OOZ OST OOT OS 0 July 2018 A-70 olsen associates, inc. ■ 'Iwo mm mmm mmm mmm mmm mmm mmw'� mmyrA mmin mmtv MMYR MIRM MFdOwl 0 0 0 0 0 (V r-1 ri N (4n9N-Iaa3) uoLIena13 OOVZ OOE'z OOZ'z OOVZ 000'z 006'T 008'T OOL'T 009'T v OOS'T v OOti'T v 00£'T m E OOZ'T v OOT'T 000'T 006 N 008 0 OOL 009 OOS OOti 00£ OOZ OOT 0 1 0 p L L U 1 II I s o o 1 17 O H � a�—I � � N � 1 •1 � I I N E E .n O to z z¢ z o J , I I I I I I I � '• �� 1 . I It II , 11 too: ' ! ,, ' I 1, 1 , 1 1 •, - y 1 r ' 1 1 1 1 1 1 1 1 1 1 •, 1 I h ' ' 1 1 1 1 TF<F-F 1111 1 TLTT 1,11111111pill 1n 0 1n 0 1n 0 Ln 0 1n N N r H �1 ' r-I r-1 (dn9N-100j) uo •en013 Figure A-70: Measured beach profiles at baseline Station 224+80, Bald Head Island, N.C. 008 OSL OOL OS9 009 OSS v Osv CO 00-V OSE 41 0 OSZ OOZ OST OOT OS 0 July 2018 A-71 olsen associates, inc. APPENDIX B PHOTOGRAPHIC DOCUMENTATION OF EXISTING STABILIZING STRUCTURES LOCATED ON WEST BEACH AND SOUTH BEACH September 2018 Terminal Groin Location Completed Bald Head Island Terminal Groin (March 3, 2016) Detached Breakwaters —Row Sheet Pile Groin (4 Boat 4_ - -`� West Jettie- Boat /Row Ai& _ L O 20 A �' � MIN. r r LANDWARD END �r GEOTEXTILE UNDERLAYER (SCOUR APRON) 18" TOE TUBE INTEGRAL TO d } SCOUR APRON (MUST BE FILLED) o M 8 V z �.0 J MID -LENGTH z O C7 NOTE: FILL PORTS NOT SHOWN ALL TUBES ARE LINED AND COATED C SEAWARD END r PROVIDE TOE TUBE g AT END, DO NOT FILL UNLESS DIRECTED. Zo BY ENGINEER NOTE.' TAPERED TUBE WITH SPINAL SEAM GROIN PLAN ..'Awl - k ¢ .. ��. .Y,. J Typical Sand Tube Groin (13) w ESSENTIAL FISH HABITAT ASSESSMENT VILLAGE OF BALD HEAD ISLAND FPS BEACH NOURISHMENT PROJECT BRUNSWICK COUNTY, NORTH CAROLINA Prepared by: - LMG LAND MANAGEMENT GROUP a DAVEYI company 3805 Wrightsville Avenue; Suite 15 Wilmington, NC 28403 910-452-0001 Prepared for: The Village of Bald Head Island Bald Head Island, Brunswick County, NC August 2020 CONTENTS CONTENTS....... FIGURES......................................................................................................................................................... ii TABLES........................................................................................................................................................... ii APPENDICES.................................................................................................................................................. ii 1. INTRODUCTION.....................................................................................................................................3 2. DESCRIPTION OF PROPOSED ACTION...................................................................................................3 2.1 PROJECT LOCATION.......................................................................................................................3 2.2 PROJECT PURPOSE........................................................................................................................6 2.3 APPLICANTS PROPOSED ACTION..................................................................................................6 2.4 ALTERNATIVE SAND SOURCE SITES...............................................................................................9 3. AVOIDANCE AND MINIMIZATION MEASURES....................................................................................18 4. POST -CONSTRUCTION MONITORING.................................................................................................20 5. ESSENTIAL FISH HABITAT DESIGNATION.............................................................................................21 5.1 MAGNUSON-STEVENS FISHERY CONSERVATION AND MANAGEMENT ACT (MSA) ...................21 5.2 DESCRIPTION OF EFH CATEGORIES IN VICINITY OF PROJECT AREA............................................23 5.2.1 ESTUARINE AND MARINE WATER COLUMN.......................................................................23 5.2.2 SOFT BOTTOM.....................................................................................................................24 5.2.3 HARD BOTTOM...................................................................................................................26 6. MANAGED SPECIES.............................................................................................................................26 7. ASSESSMENT OF IMPACTS TO ESSENTIAL FISH HABITAT....................................................................31 7.1 ESTUARINE AND MARINE WATER COLUMN...............................................................................33 7.2 SOFT BOTTOM.............................................................................................................................35 7.2.1 SURF ZONE..........................................................................................................................36 7.2.2 FRYING PAN SHOALS...........................................................................................................36 7.3 HARD BOTTOM...........................................................................................................................41 8. IMPACT SUMMARY FOR ESSENTIAL FISH HABITAT.............................................................................41 9. REFERENCES........................................................................................................................................44 Essential Fish Habitat Assessment — August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina i FIGURES Figure1. Project Location.............................................................................................................................4 Figure 2. Sand Source Location.....................................................................................................................5 Figure 3. Sand Placement Location...............................................................................................................8 Figure 4. Approximate locations of alternatives evaluated for potential sand source sites ......................10 TABLES Table 1. Dredged Material Quantities from Wilmington Harbor Project 1976-1999................................15 Table 2. Sediment Composition of Dredged Material — Wilmington Harbor Project (USACE, 2012)........16 Table 3. Categories of Essential Fish Habitat and Habitat Areas of Particular Concern in Southeast Statesl .................................................................................................................................................................... 22 Table 4. Presence of Managed Species (including life cycle stage) for Area Waterbodiesl [E=Eggs; L=Larval; J=Juvenile; A=Adult (A), N/A=Not Found]...................................................................................................28 Table 5. Summary of Potential Impacts to Essential Fish Habitat and Habitat Areas of Particular Concernl,2 .................................................................................................................................................................... 32 APPENDICES Appendix A: Design Drawings (prepared by Olsen Associates, Inc.)....... Essential Fish Habitat Assessment — August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 53 1. INTRODUCTION The purpose of this document is to present the findings of an Essential Fish Habitat (EFH) Assessment conducted per the requirements of the Magnuson -Stevens Fishery Conservation and Management Act of 1976, as amended through 1996 (Magnuson -Stevens Act). The objectives of the EFH Assessment are to describe how the Applicant's proposed action may affect EFH designated by the National Oceanic and Atmospheric Administration - National Marine Fisheries Service (NOAA-NMFS) and the South Atlantic Fisheries Management Council (SAFMC), for the area of influence of the project. According to the SAFMC, EFH within the South Atlantic Bight includes all estuarine and marine waters and substrates from the shoreline to the seaward limit of the Exclusive Economic Zone (EEZ). The area of influence of the proposed action is principally the portion of Frying Pan Shoals (FPS) in the vicinity of the proposed dredge site (including open water and subtidal bottom areas) as well as the beachfront and surfzone areas of West Beach and South Beach on Bald Head Island, North Carolina. The EFH Assessment includes a description of the proposed action; an analysis of the project alternatives considered; an assessment of the direct and cumulative effects on EFH within the area of influence for the managed fish species and their major food sources; and mitigative measures intended to minimize expected project effects if applicable. 2. DESCRIPTION OF PROPOSED ACTION 2.1 PROJECT LOCATION Bald Head Island is a 3-mile long south -facing barrier island located immediately eastward of the mouth of the Cape Fear River at 33.85°N, 77.9889°W (NAD27). The island forms the southern terminus of the Smith Island complex at Cape Fear Point from which FPS extends over thirty miles southeastward into the Atlantic Ocean. Bald Head Island's east and south shorelines (East Beach and South Beach, respectively) front the Atlantic Ocean. The western shoreline (a.k.a. West Beach) is located immediately adjacent to, and fronts, the Cape Fear River entrance. The north side of the island is bounded by the Bald Head Creek estuary. The remainder of Smith Island is composed of interior tidal creeks (including Cape Creek and Deep Creek), associated tidal marsh, Middle Island, and Bluff Island. The mouth of the Cape Fear River (over one mile in width) separates Bald Head Island from the eastern end of Oak Island (or Caswell Beach). Figure 1 depicts the location of these islands relative to the Cape Fear River entrance channel and its associated shoal formations. FPS is a submerged extension of a large-scale cuspate foreland (i.e. accretional feature formed by processes of longshore drift and prevailing wind and wave conditions). The shoals extend over thirty miles offshore from the eastern end of Bald Head Island. Geotechnical evaluations of sediments within Frying Pan Shoals were conducted by the USACE as part of the General Reevaluation Report (GRR) for this 50- year project. The findings of these analyses were reported in the Brunswick County Beaches Renourishment Study (Catlin 2010). Vibracore borings indicated that the Frying Pan Shoal borrow area identified in the GRR contained substantial volumes of sand compatible with the native beach material (Catlin 2010). Essential Fish Habitat Assessment — August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 3 Figure 1. Project Location Olsen Associates, Inc. (OA) has identified a viable sand source (i.e. borrow site) along the west side of the shoal approximately 1 mile seaward of the southeastern shoreline of Bald Head Island (Olsen Associates, Inc. 2016) (Figure 2). As part of that sand search investigation, Geodynamics performed a hydrographic survey of the area of interest (since NOAA charts are inaccurate in this dynamic area). Similarly, Tidewater Atlantic Research, Inc. (TAR) performed two phases of a marine cultural resource investigation to discern the location of potential wrecks. The Phase II investigation identified one small buffer area mapped around one cluster of magnetic anomalies (TAR 2016). Accordingly, the project design has delineated a 9.73-acre Exclusion Zone within the borrow site based upon the TAR findings. Essential Fish Habitat Assessment — August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 4 4 Figure 2. Sand Source Location Essential Fish Habitat Assessment — August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 5 Athena Technologies was retained to obtain multiple VIBRACORES within the proposed area of interest. Those cores have been logged and analyzed for sand quality. CA subsequently completed a summary report of the sand search investigation (Olsen Associates 2016). According to this report, the grand mean sand content for composite samples from the proposed borrow site was 92.09%, and the percent fines measured over depth (to -25 ft MLW) was low (2% on average). It can be reasonably expected based upon these results and the findings of other geotechnical investigations in similarly occurring, nearby shoal features that depositional sediments above a certain elevation within the defined borrow area will be of beach quality. The continuity of the predicted horizon of sands above either clay or silty sands is highly predictable at this location (Olsen Associates 2016). The permit request seeks authorization to dredge above that horizon. 2.2 PROJECT PURPOSE The purpose of the Village of Bald Head Island FPS Beach Nourishment Project is to address on -going and chronic erosion along South Beach and West Beach and to thereby protect public infrastructure, roads, homes, beaches, recreational assets, and protective dunes. Severe erosion has been chronicled along South Beach (particularly its western reach) since the 1970s. Under the most recent detailed physical monitoring, Olsen Associates, Inc. (2016) reported that the Island's gross volumetric loss (excluding East Beach) over the November 2000 to May 2016 timeframe was approximately 5.733 Mcy (corresponding to an average annualized loss of 371,700 cy). The highest rates of sand loss have occurred principally at the west end of South Beach in the vicinity of the Cape Fear River entrance. This prompted the Village of Bald Head Island (Village) to procure authorizations for, and subsequently construct, a 1,300-If terminal groin at this location. Construction of the terminal groin structure was completed in December 2015. While the terminal groin addresses chronic shoreline losses along western South Beach, it has been documented that the terminal groin and existing sand tube groin field are not sufficient, in and of themselves, to prevent or to adequately offset sand losses from South Beach or West Beach. As a result, periodic nourishment through both the federally -sponsored Wilmington Harbor dredge and disposal project and Village -sponsored projects are required to mitigate erosion along the entirety of South Beach and West Beach. The threat to existing homes, dunes and infrastructure as a result of the erosion and shoreline recession has prompted the Village to seek longer term beach nourishment options. Predicted sand volume needs for South Beach and West Beach were identified in the terminal groin EIS (for both the terminal groin alternative and non-structural alternatives). FPS was identified at that time as a long- term sand source with the potential to satisfy the sand volume requirements for South Beach and West Beach in the future. 2.3 APPLICANTS PROPOSED ACTION In order to plan for and address expected sediment deficits over the next several decades, the Village of Bald Head Island identified an approximate 460-acre area consisting of beach -compatible material suitable for placement along the South Beach shoreline (refer to Figure 3). The proposed action is for the use of an approximate 198-acre dredge site (portion of the 460-acre area of interest) with a predicted Contract volume of 2.5 Mcy of beach fill (including losses experienced during dredging and fill placement). This borrow site to be permitted is located on the western portion of the Frying Pan Shoals formation approximately 1 mile off the southeast shoreline of Bald Head Island. Sediment identified within the Essential Fish Habitat Assessment —August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 6 Frying Pan Shoals borrow site will be excavated by cutter suction dredge and pumped by submerged pipeline to the South Beach shoreline. Assuming a neat sand volume to a depth of -20 ft NAVD88, the identified borrow site could theoretically yield up to 2.487 Mcy. To an elevation of -25 ft NAVD88, the neat sand volume is estimated to be 3.995 Mcy. Within the requested 198.4-acre borrow site there is included a 9.73-acre Exclusion Zone intended to avoid impact to potential cultural resources as identified by T.A.R. As a result, the net area available for dredging is 188.7 acres. Pragmatically, it is expected that the Contractor's Dredge Plan submitted prior to construction could reduce the actual spatial acreage dredged by up to 25%. Refer to Appendix A for the design drawings of the proposed action (including plan view drawings of the proposed borrow site). The South Beach construction fill template will maintain an approximate average berm elevation of +8 ft. NGVD which is consistent with prior beach fill berms constructed by the Wilmington District USACE and the Village since 2001. A mild slope in the seaward direction will be introduced into the berm (by grading) to reduce post -placement scarping and enhance post -construction turtle nesting activities. Should dune erosion or benching be evident at the time of construction, up to 5 cy of sand per ft. of shorefront would be mechanically moved and graded to repair the duneline. As in the past, any revegetation necessary for dune stabilization will be performed by the Village under separate contract subsequent to fill placement completion by the dredge contractor. Post -construction beach tilling will be performed based upon consultation with Resource Agencies after each future fill event. To -date however, that requirement has been waived after an on -site evaluation by agency personnel. It can be reliably assumed that a 27"-30" cutter suction dredge (Ocean Certified) must be utilized to excavate material from the permitted open water site. Both draft and operational (as well as safety) considerations for such dredge plants necessitate depths of excavation exceeding -15 ft (MLLW datum). Essential Fish Habitat Assessment — August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 7 QNSLOWBR Y 5 �r a z W CAK FEAR t � 1 r J J+ f LFRY ING PAW. SHOALS —FILL LENGTH: 17,200 FT 0 . A TLAN-nC OCEAM LIMITS OF FUTURE PROJECT RELATED FILL ACTIVITIES BY VILLAGE UTILIZING FRYING PAN SHOALS BORROWSITE CAPE F4EAR y Rl VEIL i . G ROIN J OGTOBER 2416 PHOTOGRAPHY Figure 3. Sand Placement Location Essential Fish Habitat Assessment — August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina E3 2.4ALTERNATIVE SAND SOURCE SITES Areas considered as potential sources of suitable material for beach nourishment have been evaluated in the context of the project requirements (both in terms of sand quality and quantity). Generally, sand source areas must consist of sediments satisfying minimum standards for beach fill projects as stipulated by the North Carolina Administrative Code (15A NCAC 07H.0312 Technical Standards for Beach Fill Projects)'. The applicant must also consider the proximity of the source area relative to the area of beach being nourished due to transport logistics, project duration, constructability, and cost constraints. All dredging and beach filling operations must be confined to a relatively narrow window of time to minimize potential adverse effects to environmental resources. In light of these considerations, the most desirable potential sources are identified in the general vicinity of West Beach and South Beach on Bald Head Island. The Applicant, in coordination with the project engineer, evaluated several borrow site alternatives prior to the design of the proposed Frying Pan Shoals borrow site. The initial analysis of alternative borrow sites was used to help identify the least environmentally damaging, practicable alternative (LEDPA) in accordance the National Environmental Policy Act (NEPA). The alternatives analysis has been updated for the purpose of this EFH Assessment. The following sites were considered as part of the alternatives analysis: (1) Nearshore Inlet Shoals (including Jay Bird Shoals and Middle Ground); (2) Wilmington Harbor Entrance Channel (Inner Three Reaches); (3) Bald Head Creek Shoal Complex; (4) Offshore Ocean Dredged Material Disposal Site (ODMDS); (5) Confined Disposal Facilities; and (6) Frying Pan Shoals. The approximate locations of alternatives evaluated for potential sand source sites are depicted in Figure 4. t Notably, Frying Pan Shoals (FPS) is exempt from the sediment criteria rules. SL 2017-10 specifies that until the North Carolina Coastal Resource Commission (CRC) adopts rules exempting cape shoal systems from the Sediment Criteria Rule, it is required to "exempt from the permitting requirements of the Sediment Criteria Rule and any sediment in the cape shoal systems used as a borrow site and any portion of an oceanfront beach that receives sediment from the cape shoal systems," including from FPS. SL 2017-10 section 3.15(b) and (c). Essential Fish Habitat Assessment —August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 9 N I --N z / o CO L T y f W N N � N r � � y yy K r3 17 f U � r . N F sr f 'gJ N 0O LL a I— � � f6 L „ LL i Figure 4. Approximate locations of alternatives evaluated for potential sand source sites Essential Fish Habitat Assessment — August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 10 Alternate Borrow Areas within Nearshore Inlet Shoals (including Jay Bird Shoals and Middle Ground) In January 2017, the Village submitted state and federal permit applications for the proposed dredging of a borrow site on Frying Pan Shoals (FPS). In consideration of the concerns raised by National Marine Fisheries Service (NMFS) and their accompanying recommendation to first explore other viable sand - source alternatives, the Village further evaluated the potential to prioritize the use of the previously authorized borrow site located on Jay Bird Shoals (JBS) (including both the partially recovered area dredged in 2009 and any remaining, undredged portions of the permitted borrow site at that time). The Village had identified the JBS borrow site as the only other viable alternative borrow area available for near term sand placement at Bald Head Island (BHI). From an operational and cost standpoint there is preference to utilize the previously authorized and dredged JBS site. That being said, the Village utilized this site for a second time in its most recent Village - sponsored nourishment project (occurring in Winter 2018/2019). This project included the dredging and placement of 1.21VIcy of sand on South Beach. Sand reserves within the JBS permitted site were sufficient to meet the nourishment volume required for the 2018/19 project; however, dredging beyond the previously developed borrow site limits could eventually induce significant impacts to the JBS shoal feature. More expansive dredging within the JBS and Middle Ground feature could affect wave climate and tidal flows to such an extent that that it could adversely impact the shoreline of Caswell Beach and Fort Caswell on Oak Island, as well as West Beach on Bald Head Island. The Town of Oak Island recently completed investigations and modeling of the proposed use of JBS and Middle Ground for nourishment of the Oak Island shoreline. Based upon vibracore data and modeling results, the Town's engineer identified an approximate 304-acre borrow site within JBS as the least environmental damaging, practicable alternative for that project. Authorizations for the Town of Oak Island to dredge this borrow site were recently issued by the Corps of Engineers and the NC Division of Water Resources (April 2020). Use of other areas on JBS and Middle Ground were excluded from consideration either due to not having sufficient volumes of beach -compatible material or for the increased potential for adverse physical impacts to the shoreline of Fort Caswell and the Town of Caswell Beach (by way of alterations to tidal currents or wave transport). As part of the authorization for the 304- acre JBS borrow site, a Technical Advisory Committee (TAC) has been established and will be engaged if it is believed that the authorized project is causing unintentional effects on Caswell Beach. In consideration of the recently constructed Village -sponsored nourishment project (2018/2019) and the recently authorized Town of Oak Island project, use of JBS as a potential sand source site is not viable for the foreseeable future. Additional removal of material from these two areas to offset sand losses on Bald Head Island (or Oak Island) would provide temporary benefits at best with the likelihood of reducing beneficial effects in their lee on one or both of the two adjacent barrier islands. Hence, "over -utilization" of these potential sand sources is not recommended and, in all probability, would be strongly opposed by interests on the east end of Oak Island. However, the borrow site previously permitted for Village - sponsored projects is continuing to be physically monitored on an annual basis. If the shoreline of South Beach can be maintained though federal nourishment for a period of time and sufficient physical recovery occurs within JBS prior to the next nourishment need, then the Village will seek to utilize JBS as an alternative sand source site prior to the use of FPS. Physical monitoring of the JBS borrow site will determine the volume of sand available for dredging prior to the next Village -sponsored nourishment, and this information will be provided to the agencies to determine if JBS can be utilized in lieu of FPS. Essential Fish Habitat Assessment —August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 11 Similar to JBS and Middle Ground, Bald Head Shoal is a depositional feature that generally exhibits high sand content in sufficient quantities to provide the necessary amount of nourishment to offset the sand losses on South Beach under consideration. However, this shoal plays a critical role in the dissipation of storm wave energy affecting the beaches along Oak Island and Bald Head Island. In addition, the shoals provide intertidal and subtidal habitat supporting estuarine and marine fauna. Furthermore, these areas as inlet associated shoals are identified as HPAC. Dredging from Bald Head Shoal is predicted to be highly detrimental considering ongoing changes at that nearshore location due to the navigation channel reorientation, as well as the proximity and important beneficial sheltering effects of this depositional feature to the currently eroding Bald Head Island beaches. Use of this shoal as a sand source site would result in the need for increased frequency of nourishment events, a condition not deemed environmentally favorable nor operationally and financially practicable. It can therefore be excluded from consideration as a viable sand source site for the proposed project. Wilmington Harbor Entrance Channel By way of Permit Condition #60 of Department of Army (DA) Authorization of the Terminal Groin Project (Action ID No. SAW-2012-00040), the Village must evaluate the Wilmington Harbor Entrance Channel as a potential borrow site for the maintenance of the groin fillet. To that end, the Village evaluated the use of the federal channel reaches for borrow material as part of the Village -sponsored 2018/19 beach nourishment project. Since all sand dredged by the Corps of Engineers (COE) in 2017/18 as part of their regularly occurring channel maintenance was placed on Oak Island pursuant to the Wilmington Harbor Sand Management Plan (WHSMP), there was not sufficient sand quantities available to the Village for their project. Similarly, the timing of future COE channel maintenance projects makes it difficult to design, permit, and contract a Village -sponsored project within the federal channel with any level of certainty of sand volumes and locations. This assessment was corroborated by the Wilmington District Engineering staff as part of a Section 408 Permit analysis in May 2018 required bythe Villages' 20191.2 Mcy fill project. At that time, the District determined that dredging of the navigation channel was not a "practicable" option for beach maintenance on Bald Head Island. Moreover, pursuant to the WHSMP, the navigation channel disposal sand is presently scheduled for episodic placement on Oak Island beaches every third maintenance event. Bald Head Creek Shoal The previously permitted and dredged borrow site of the ebb tidal shoal of Bald Head Creek (BHC) is limited in size and sand volumes to be able to address long-term sand needs of South Beach. Given its location and relatively small quantity of sand available and the shallow depth of dredging required at that location, the BHC borrow site is better suited for small volume requirements at West Beach. Moreover, only a small shallow draft dredge can be utilized at that location. Therefore, the Bald Head Creek site is not suitable for any large-scale nourishment event on South Beach. Areas within Former Federal Channel Offshore sediment data acquired from areas situated within the former federal channel alignment at the mouth of the Cape Fear River indicate a high content of fine sediments generally considered unsuitable for beach nourishment. Due to the nature of this depositional material and the technical standards for beach placement, this alternative is determined not to be practicable and is therefore eliminated from further consideration. Essential Fish Habitat Assessment — August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 12 Offshore ODMDS The offshore ODMDS has been used for the disposal of dredged materials from the Wilmington Harbor Federal navigation project and the Military Ocean Terminal at Sunny Point (MOTSU) for many decades. MOTSU is a military port facility located on the west bank of the Cape Fear River approximately 10 miles upstream from the river's mouth. Both the Federal navigation project and MOTSU require some level of annual maintenance dredging. Reaches of the Federal project maintenance extend from the ocean bar channel at the mouth of the Cape Fear River to a point just north of Smith Creek on the Northeast Cape Fear River (north of Wilmington, NC). The Wilmington Harbor Dredged Material Management Plan (DMMP) provides specific information as to the historical and present-day use of the ODMDS including documentation of the quantity and character of material placed within. In addition, an evaluation of potential beneficial uses of material dredged from the Federal navigation project is required as part of the DMMP. This requirement served as the premise for the establishment of the 2000 Wilmington Harbor Sand Management Plan (SMP) which specifically provides for the return of littoral material to the beachfront. According to the SMP, beach -compatible dredged material (sands) dredged from the ocean bar or river navigation channel should be placed on nearby beaches or within the active littoral system when it is economically and environmentally acceptable to do so. The DMMP clearly documents conditions of the two ODMDS sites (both the old site used until 2002 and the new site used for current dredged material disposal). Specific volume totals of dredged materials placed within the former ODMDS site are available from 1976 through 1999 (Table 1). Since 1987, the date of the site designation, approximately 27.6 Mcy of dredged materials have been placed within the ODMDS. The source of the material is divided into three general zones within the Cape Fear River: (1) the Wilmington Harbor Federal navigation project, ocean bar channels (WH-OB); (2) the Wilmington Harbor navigation channel to Wilmington, excluding the ocean bar and portions above the Lower Brunswick channel (WH-NAV); and (3) the MOTSU channel. Of the total material disposed in the ODMDS, approximately 15.5 Mcy (56%) of the material has come from WH-NAV and the MOTSU channels. As identified in Essential Fish Habitat Assessment — August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 13 Table 2, the mid -project reaches of WH-NAV and MOTSU exhibit significantly higher silt and clay components not compatible with beach placement. MOTSU dredged material alone (accounting for 12 Mcy or 43% of the total material placed in the ODMDS since 1987) is characterized as silty riverine sediments consisting of 70% silt and clay. Additionally, it is commonly reported that the ODMDS consists of woody debris associated with prior dredging of the river bottom. Since the development of the Sand Management Plan (as part of the Wilmington Harbor Deepening Project in 2000), beach compatible sand dredged during maintenance events has been pumped to the shorelines of Bald Head Island and Oak Island. As a result, much of the material disposal at the new ODMDS location consists of higher silt and clay content. In light of these documented conditions, use of either the old or the new ODMDS sites has been determined to be not practicable and has been eliminated from further consideration in the following analysis of potential actions. Essential Fish Habitat Assessment — August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 14 Table 1. Dredged Material Quantities from Wilmington Harbor Project 1976-1999. DREDGED MATERIAL QUANTITY - CUBIC YARDS YEAR WH-OB WH-NAV MOTSU YEAR TOTAL 1976 1,157,161 0 0 1,157,161 1977 218,624 0 0 218,624 1978 523,803 0 0 523,803 1979 138,817 0 0 138,817 1980 951,935 0 0 951,935 1981 376,942 0 0 376,942 1982 850,621 0 0 850,621 1983 1,018,839 0 0 1,018,839 1984 1,297,202 0 0 1,297,202 1985 190,633 0 0 190,633 1986 756,423 0 0 756,423 1987 1,571,976 0 983,250 2,555,226 1988 0 597,568 0 597,568 1989 1,124,408 0 1,255,134 2,379,542 1990 524,267 0 1,047,290 1,571,557 1991 427,176 466,349 0 893,525 1992 1,051,328 0 773,950 1,825,278 1993 749,800 0 945,255 1,695,055 1994 1,040,600 0 549,770 1,590,370 1995 1,594,295 1,633,852 398,111 3,626,258 1996 1,000,000 345,430 3,683,330 5,028,760 1997 1,444,000 217,294 132,914 1,794,208 1998 901,988 196,442 1,473,582 2,572,012 1999 675,549 0 825,000 1,500,549 1976-1999 19,586,387 3,456,935 12,067,586 35,110,908 1987-1999 12,105,387 3,456,935 12,067,586 27,629,908 Note: WH-OB - Baldhead Shoal through Battery Island Channels, inclusive. WH-NAV - Lower Swash through portions of Lower Brunswick channels. MOTSU - Materials associated with MOTSU only. Material Management Plan (DMMP) Wilmington Harbor, North Carolina, June 1996. U. S. Army Corps of Engineers, Wilmington District - Ocean Disposal Database and Contract Dredging Records. Essential Fish Habitat Assessment - August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 15 Table 2. Sediment Composition of Dredged Material - Wilmington Harbor Project (USACE, 2012) Channel %Gravel % Sand % Silt & Clay Sediment Grouping Bald Head Shoal Offshore Reaches 0.0 73.2 26.8 Silty Offshore Inlet Reaches 0.0 98.7 1.3 Sandy Lower Project Reaches Smith Island 7.9 92.0 0.1 Caswell -Southport 18.0 80.5 1.5 Southport 12.5 85.5 2.0 Battery Island 38.0 61.0 1.0 Lower Swash 27.0 70.0 3.0 Horsheshoe Shoal 0.0 98.0 2.0 Reaves Point 0.0 99.0 1.0 Lower Midnight 0.0 76.0 24.0 Varied Mid -Project Reaches Upper Midnight 0.0 82.5 17.5 Lower Lilli ut 0.0 56.5 46.5 Upper Lilli ut 0.0 98.0 2.0 Keg Island 0.0 63.0 37.0 Upper and Lower Big Island 2.0 94.0 3.0 Lower Brunswick 0.0 92.7 7.3 Upper Brunswick 0.0 57.0 43.0 Fourth East and Between 0.0 80.0 20.0 Anchorage Basin 0.0 6.0 94.0 Silty Upper - Project Reaches Between Memorial & Hilton Railroad Bridges 10.0 55.0 35.0 Above Hilton Railroad Bride 0.0 58.0 42.0 MOTSU* 0.0 30.0 70.0 Silty Riverine Note: Gravel - grain size larger than 5.0 mm Sand -grain size between 0.07 and .5 mm Silt and Clay -grain size smaller than 0.07 mm Source: USACE 1996 except for * which is USACE 1993 Essential Fish Habitat Assessment - August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 16 Confined Disposal Facilities (CDFs) Over the years, maintenance for the Wilmington Harbor project has resulted in the creation of disposal sites along channelized reaches of the Cape Fear River Estuary. The 1989 Environmental Impact Statement (EIS) for the long-term maintenance of Wilmington Harbor (USACE 1989) identified eighteen (18) disposal sites extending from Snow Marsh Channel (north of Southport) to near the upstream limit of the federal project on the Northeast Cape Fear River (just north of the mouth of Smith Creek) (refer to Attachment A). The disposal areas were originally formed from pumping material to unconfined areas along maintained channel reaches. Over time, the federal project included the construction of upland dikes to contain the dredged material. Most of these diked upland facilities have since been abandoned by the USACE. These areas range in size with all but one site (Area 15 on Eagles Island) less than 50 acres. Many of the sites have eroding dikes and have been subsequently overgrown by Phragmites australis and wetland plant species. Based upon the location of these areas, many of the sites consist of mixed material with higher content of fine-grained sediments. Only two sites (Area 3 and Area 4) are still maintained by the USACE as CDFs. Area 3 (29 ac) has mixed sediment content and would likely not be a suitable source candidate for beach quality material. Area 4 (25 ac) consists predominantly of beach -compatible sand. However, sand from this island is dedicated for the federally -authorized Kure Beach project in New Hanover County (NC). Based upon documentation of existing disposal areas of the Wilmington Harbor project, use of any single CDF as a source of beach -compatible sand is not viable. All but one of these sites consists of mixed sediment content deemed unsuitable for beach placement. The one CDF (Area 4) that contains higher percent sand content is dedicated as a sand source for the federally -authorized Kure Beach project. Given the quantity of sand required for nourishment on Bald Head Island, the State technical standards the material must meet, and issues associated with constructability, CDFs are not considered a practicable sand source alternative. Frying Pan Shoals (Applicant's Preferred Alternative) The screening and identification of a suitable borrow site considered the following conditions: • documented strata of high -quality beach compatible sediment suitable for meeting both State Standards and post -placement performance criteria acceptable to the Engineer and the project Sponsor (and in quantities sufficient to nourish the entirety of South Beach); • desirable constructability characteristics for purposes of sand excavation and beach fill construction by an ocean -certified cutter suction dredge; • avoidance of cultural resources necessary for operational feasibility, and • siting of the borrow area in a known dynamic but highly depositional area for purposes of ensuring rapid substrate recovery; • siting of the borrow area to minimize biological impacts to resident and transient species and their habitats (including Essential Fish Habitat); and • reasonable accessibility to Bald Head Island and proximity to nourishment site for logistic and cost considerations (i.e. the project must be practicable and not prohibitively expensive). In light of the criteria identified to meet the Applicant's project purpose and need, use of a potential borrow site beyond three nautical miles (i.e. in federal waters) would not be feasible. In particular, such a site would not provide reasonable accessibility to the nourishment site (needed for operational benefits), would be cost prohibitive, and would necessitate working outside of acceptable environmental windows. In addition, it would require the use of a hopper dredge that would result in entrainment Essential Fish Habitat Assessment —August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 17 impacts to fish and sea turtles as well as increased risk of collision with protected cetaceans. As a result, Olsen Associates, Inc. (OAI) identified a nearshore candidate sand source (i.e. potential borrow area) on Frying Pan Shoals that is further described below as the Applicant's preferred alternative. In addition, more detailed information regarding existing conditions and proposed work is provided. OAI has identified a preferred borrow site location (consisting of an evaluation area of approximately 460 acres and a dredge site of approximately 198 acres) along the west side of Frying Pan Shoals approximately 1 mile seaward of the southeastern shoreline of Bald Head Island. Frying Pan Shoals is a submerged extension of a large-scale cuspate foreland (i.e. accretional feature formed by the historical deposition of a longshore drift originating from both the north and the west). The shoal formation extends well over thirty miles offshore from the eastern end of Bald Head Island. Prior federal studies have identified the presence of vast quantities of beach -quality sand throughout much of the shoal formation. The Village recently initiated more detailed site investigations (including hydrographic surveys, geotechnical investigations, and marine cultural resource surveys). Based upon these studies and subsequent engineering analysis, the identified borrow site has been further refined to an approximate 198.4-acre area (refer to Permit Sheet 7 of 9, Appendix A). Avoidance and minimization measures are further described in Section 3 below. 3. AVOIDANCE AND MINIMIZATION MEASURES The selection of the proposed Phase I Bald Head Island 198.4-acre borrow site met the identified screening criteria outlined above and capitalized on the findings of hydrographic surveys, geotechnical investigations, and two phases of cultural resource investigation. The specified design depth of the proposed borrow site will ensure that substrate sediments exposed immediately after project construction will continue to consist of high -quality sands. Borrow site "recovery" (i.e. infilling) will initially be influenced by both slumping of excavation perimeter side slopes and rapid deposition from predictable sediment transport from north to south along the marginal shoal feature — as presently exists today. Advance quantification of infilling rates is difficult due to equilibration processes between cut and uncut portions of shoal during the first few years following dredging. Consequently, physical monitoring of the borrow site recovery will be performed. It is well documented, however, that the section of shoal in question is naturally depositional both in the modern day and the morphological sense. Regardless of future realized sediment deposition rates, the probability of sedimentation by similar sandy material (in contrast to fines, organics, clays, etc.) is excellent (McNinch, 2009) and coincidently is the principal post -construction borrow site characteristic desired for purposes of rapid recovery of benthic communities (Bergquist, et.al. 2008) and corresponding minimization of potential adverse effects to Essential Fish Habitat (EFH). The project as designed will incorporate the following protection measures identified by the South Atlantic Fisheries Management Council (SAFMC) specific for dredge and fill projects in areas designated as Habitat Areas of Particular Concern (HAPC). These include the following: 1. Impact assessment (description of potential impacts; baseline information; alternatives analysis; construction monitoring; post -construction monitoring plan); 2. Fill material should match that of recipient beach as closely as possible; Essential Fish Habitat Assessment — August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 18 3. Dredging to be located in areas characterized by strong currents and sand movement to promote more rapid infilling rates (and thus reducing the duration of impacts to benthic habitats); and 4. Dredging should be performed in a manner intended to minimize impacts to wave energy and currents, "thus reducing the likelihood of infilling with fine-grained sediments" In addition to the SAFMC protection measures, the proposed project incorporates following design elements that helps to further reduce or avoid impacts to natural resources: 1. The site is a highly dynamic and renewable shoal feature (maintained by seaward flow of current off cape) and thus physical and biological disturbances tend to be short-lived; 2. The position of borrow site on the western flank represents a sediment sink (thus promoting rapid recovery and infilling with like material); 3. The combination of size and position of sand source site results in least impacts to shoal integrity; 4. Dredging to occur during winter months (reduced biological activity); 5. The project will allow for undredged areas in close proximity to be left undisturbed to promote more rapid recolonization of benthos (as was documented for Jay Bird Shoals and Bald Head Creek Shoals with similar post -project conditions); 6. The project will avoid hard -bottom habitat; 7. The project will avoid Primary Nursery Area (PNA) impacts; 8. The project will avoid inlet and associated shoals for large-scale sand volume needsz; 9. The project will utilize hydraulic cutter suction dredge (thereby avoiding and minimizing physical entrainment of species in close proximity to the dredge operation); and 10. The project will include post -project physical monitoring of borrow site (i.e. assessment of physical recovery). Attributes of the borrow site location and design as described above help to minimize both physical and related ecological effects. The Applicant and project engineer have worked to further reduce the limits of spatial impacts of the proposed borrow site based upon comments received subsequent to the submittal of the 2016 proposal. Of particular note with respect to avoidance and minimization efforts since the 2016 submittal is the following: the deletion of the dredge access corridor (aka "fairway"); the reduction in borrow site acreage (from 460.1 acres to 198.4 acres); and the limitation of dredging to an initial single borrow event to be monitored. In addition, the Applicant continues to monitor the physical recovery of the Jay Bird Shoal (JBS) borrow site on an annual basis. If the shoreline of South Beach can be maintained though federal nourishment for a period of time and sufficient physical recovery occurs within JBS prior to the next nourishment need, then the Applicant will seek to preferentially utilize JBS as an alternative sand source site prior to the use of FPS. Physical monitoring of the JBS borrow site will determine the volume of sand available for dredging prior to the next Village -sponsored nourishment, and this information will be provided to the agencies to determine if JBS can be utilized in lieu of FPS. As indicated above, the permit request is for a one-time dredge event with both physical and benthic monitoring proposed to evaluate the effects of dredging on FPS prior to any requests for dredging in the future. The Applicant acknowledges the need for the monitoring of physiographic, sedimentary and 2 All coastal inlets are designated HAPC for paneaid shrimp, blue crabs, and estuarine -dependent snapper -grouper species. Essential Fish Habitat Assessment —August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 19 benthic recovery within the proposed area of excavation. VHBI's engineer (Olsen Associates) believes that based upon the existing precepts of the Wilmington Harbor Sand Management Plan, which episodically places high quality maintenance sand on BHI, it could be necessary to construct an interim locally sponsored beach fill project on 8- to 12-year intervals (more or less). However, the use of JBS for future events could very well provide a viable alternate sand source in lieu of the FPS borrow area. 4. POST -CONSTRUCTION MONITORING The Village as Permittee shall perform physical monitoring of the dredged FPS borrow site immediately after construction, annually for three (3) years and biennially thereafter. The post -construction bathymetry will be compared annually with subsequent monitoring results to calculate in -filling or "recharge" of the site. The results of the monitoring will be incorporated into the Village's existing comprehensive Shoreline Monitoring Program and reported annually. The footprint of each monitoring survey shall include the entire permitted area plus a 500-ft buffer outside the site. No changes in morphology to the Frying Pan Shoals formation is anticipated; however, changes in bathymetry throughout the study area as well as proximate to any cultural resource buffer will be monitored. In addition, both sediment substrate and benthic infaunal sampling will be performed before dredging and once annually post -dredging for a period of three years. Sediment samples will be analyzed by a certified laboratory for analysis of percent organic matter and particle size distribution/texture (percent sand, silt, and clay) in accordance with ASTM standards. Benthic sampling will be performed via grab samples of both reference (undisturbed) transects and dredge transects. All samples will be sorted and identified to the lowest taxonomic level possible (generally species) and counted. Essential Fish Habitat Assessment — August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 20 5. ESSENTIAL FISH HABITAT DESIGNATION 5.1 MAGNUSON-STEVENS FISHERY CONSERVATION AND MANAGEMENT ACT (MSA) The 1996 amendments of the Magnuson -Stevens Fishery Conservation and Management Act (MSA) mandate the identification and maintenance of habitats essential to the development and support of fisheries. Essential Fish Habitat (EFH) is identified as "those waters and substrate necessary to fish for spawning, breeding, feeding, or growth to maturity" (MSA § 3(10)). The MSA amendments provide guidelines for the incorporation of EFH provisions into Fishery Management Plans (FMPs) developed by NOAA Fisheries and applicable regional Fishery Management Councils (FMCS). For the purpose of interpreting the definition of EFH, "waters" include aquatic areas and their associated physical, chemical and biological properties that are used by fish and may include aquatic areas historically used by fish where appropriate; "substrate" includes sediment, hard bottom, structures underlying the waters and associated biological communities; "necessary" means the habitat required to support a sustainable fishery and the managed species' contribution to a healthy ecosystem; and "spawning, breeding, feeding, or growth to maturity" covers a species' full life cycle. EFH is described by the Councils in amendments to FMPs, and is approved by the Secretary of Commerce acting through NOAA Fisheries (50 CFR §600.10). Section 305(b)(2) of the MSA requires all federal agencies to consult with the Secretary on all actions or proposed actions authorized, funded, or undertaken by the agency that may adversely affect EFH. Procedures developed to address EFH coordination, consultation and recommendation requirements are identified in 50 CFR § 600.905-930. Additional consultation guidance was developed by the National Marine Fisheries Service (NMFS) Office of Habitat Conservation (NMFS 2010). EFH that are considered particularly important to the long-term productivity of a managed species or to be particularly vulnerable to degradation have been defined as Habitat Areas of Particular Concern (HAPC). The EFH provisions authorize the NOAA — NMFS and Regional Fishery Management Councils (FMCS) to provide consultation and conservation recommendations on proposed projects that may adversely affect EFH and HAPC either directly or indirectly. The Fishery Management Plan (FMP) Amendments of the SAFMC have targeted specific categories of EFH and HAPC as depicted in Table 3. Coastal inlets and areas of submerged aquatic vegetation (SAV) are identified as HAPC for several managed species. Essential Fish Habitat Assessment — August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 21 Table 3. Categories of Essential Fish Habitat and Habitat Areas of Particular Concern in Southeast Statesl Essential Fish Habitat Geographically Defined Habitat Areas of Particular Concern Estuarine Areas Area -Wide Aquatic Beds Council -designated Artificial Reef Special Management Zones Estuarine Emergent Wetlands Hermatypic (reef -forming) Coral Habitat and Reefs Estuarine Scrub/Shrub Mangroves Hard Bottoms Estuarine Water Column Hoyt Hills Soft Bottom/Intertidal Flats Sargassum Habitat Oyster Reefs and Shell Banks State -designated Areas of Importance for Managed Species Palustrine Emergent and Forested Wetlands Submerged Aquatic Vegetation Seagrass Coastal Inlets Marine Areas North Carolina Artificial/Manmade Reefs Big Rock Coral and Coral Reefs Bogue Sound Live/Hard Bottoms Capes Fear, Lookout, & Hatteras (sandy shoals) Coastal Inlets Sargassum Habitat Soft Bottom/Intertidal Flats New River Marine Water Column Ten Fathom Ledge The Point 'As identified by the South Atlantic Fishery Management Council in the Final Habitat Plan for the South Atlantic Region (SAFMC, 1998). The HAPC designation is described in the implementing regulations of the EFH provisions (50 CFR §600.815). According to the Mid -Atlantic Fishery Council (MAFMC 2016), Councils are encouraged to identify habitat types or areas within EFH as HAPCs, based on one or more of the following considerations: (i) The importance of the ecological function provided by the habitat; (ii) The extent to which the habitat is sensitive to human -induced environmental degradation; (iii) Whether, and to what extent, development activities are, or will be, stressing the habitat type; and (iv) The rarity of the habitat type. According to the MAFMC guidance (2016), the HAPC designation does not confer any specific habitat protections, but can focus habitat conservation efforts through several pathways. Councils may take HAPCs into consideration when minimizing adverse impacts from fishing, for example, through restrictions on where and when fishing activities may occur. While NOAA Fisheries and the councils lack the authority to regulate non -fishing activities, federal agencies must consult with NOAA Fisheries when authorizing, funding or undertaking activities that may adversely impact EFH (16 U.S.C. 1855 §305(b)(2)). Within the EFH consultation process, HAPCs encourage increased scrutiny and more rigorous conservation recommendations for reducing adverse impacts to fish habitat. Finally, HAPCs can serve as a tool for focusing habitat research and monitoring efforts. Categories of EFH potentially affected by the proposed action include the estuarine emergent wetlands, estuarine and marine water column, oyster reefs and shell banks and soft bottom and intertidal flats. HAPC potentially affected by the proposed action include coastal inlets and SAV. Essential Fish Habitat Assessment —August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 22 5.2 DESCRIPTION OF EFH CATEGORIES IN VICINITY OF PROJECT AREA 5.2.1 ESTUARINE AND MARINE WATER COLUMN Water column habitat is defined as "the water covering a submerged surface and its physical, chemical, and biological characteristics. The water column provides corridor and connectivity for all life stages of managed species. Species occurrence and distribution is influenced by the physiochemical parameters of the water column (principally salinity and temperature) in conjunction with location relative to inlets and habitat structure. Differences in the chemical and physical properties of the water affect the biological components of the water column, including fish distribution" (Deaton et al. 2010). The water column is considered the primary component which binds the entire coastal aquatic ecosystem connecting a complex web of influences from both land and sea [15A NCAC 07H .0206(b)]. Estuarine and marine water column EFH is present within or near the proposed project. Estuarine waters are located in the vicinity of the mouth of the Cape Fear River (i.e. in proximity to the nourishment site of West Beach). The offshore borrow site and nearshore surf zone of South Beach consist of marine waters. Impact assessment and mitigative measures for the proposed action will focus on the estuarine and marine water column present at the offshore borrow site and the nearshore waters of the surf zone of the nourishment sites (along South Beach and West Beach). Estuarine water column is described as the transitional zone located between freshwater and marine waterbodies where riverine and ocean systems mix. Nutrient mixing and fish recruitment in these estuarine water columns are primarily a function of the prevailing winds, buoyancy -driven flows, and lunar tides. Estuaries are highly productive and provide vital nursery areas and habitat for many of North Carolina's commercial and recreational fish species. Estuarine -dependent species comprise more than 90% of North Carolina's commercial landings and over 60% of the recreational harvest (Deaton et al. 2010). The Cape Fear River is the only major river in North Carolina that flows directly into the ocean which makes its estuary unique compared to others in the state. In the lower Cape Fear River estuary, lunar tides have a dominant effect on salinity variations, whereas the upper estuary (above Wilmington) is more influenced by freshwater discharge. Because of the relatively high discharge of freshwater and the low volume of the Cape Fear estuary, the flushing rate is approximately 14 days which makes it the most rapid turnover of all major estuaries in North Carolina. The water column associated with the mouth of the Cape Fear River provides a corridor for numerous estuarine -dependent species utilizing the estuary for foraging, refuge, and nursery habitat. Juvenile and adult coastal demersal species (e.g. summer flounder, red drum, and bluefish), juvenile and adult coastal pelagics (cobia, Spanish mackerel, and king mackerel), and juvenile members of the snapper -grouper complex (e.g. black sea bass, sheepshead, and gag grouper) migrate through the mouth of the Cape Fear River to and from nearshore marine waters. Marine water column are those waters overlying the continental shelf and its associated high-energy coastlines where salinities exceed 30 ppt. (Deaton et al. 2010; Cowardin et al. 1979). Lunar tidal cycles are the major mixing mechanism in the marine water column with tidal amplitudes averaging 4.3 ft near Cape Fear. Winds are also an important component to water movement and mixing in all layers of the marine water column. Winds move large water masses inshore, in turn, aiding larval transport of ichthyofauna spawned in the offshore waters of the continental shelf in their migration to the nearshore environment. Larvae have been demonstrated to exert considerable control over vertical movement within the water Essential Fish Habitat Assessment —August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 23 column (Morgan and Anastasia, 2008). Migration of larvae outside the tidal influence of the estuary is influenced through wind -driven transport and directed vertical movement by larvae to maximize shoreward movement (Boehlert and Mundy, 1988). Once nearshore, then alongshore drift is the principal mechanism until larvae reach the entrainment influence of the estuary. The surf zone water column is the principal transport corridor for larvae of marine -spawning, estuarine dependent species that migrate into the coastal inlets. In addition, the water column of the surf zone provides habitat for juveniles and adults of a number of managed species including bluefish (Pomatomus saltatrix), king mackerel (Scomberomorus cavalla), and Spanish mackerel (Scomberomorus maculatus). The offshore waters of North Carolina are uniquely suited for the occurrence of a range of species due to the convergence of the warm, north -flowing Gulf Stream and the cool, south -flowing Virginia Coastal Labrador current near Cape Hatteras. Off the southeastern shorelines of North Carolina, the Gulf Stream tends to increase water temperatures and salinities and transport fish larvae from southern areas into nearshore zones. Along shoals, there may be localized upwelling of cooler, nutrient -rich waters (Deaton et al. 2010). NOAA issued a draft amendment to update EFH for Atlantic highly migratory species (HMS) with the most recent information available (NOAA 2016). According to this report, the EFH in close proximity to the shoreline of Bald Head Island (including the offshore waters in the vicinity of FPS) was identified for the following HMS: bluefin tuna (adult); skipjack tuna (juvenile); roundscale spearfish (adult); longbill spearfish (all life stages); blacktip shark (Atlantic stock, juvenile and adult); sandbar shark (juvenile and adult); scalloped hammerhead shark (juvenile and adult); spinner shark (neonate/YOY, juvenile, and adult); tiger shark (neonate/YOY, juvenile, and adult); blacknose shark (Atlantic stock, juvenile and adult); bonnethead shark (Atlantic stock, juvenile and adult); Atlantic sharpnose shark (neonate/YOY, juvenile, and adult); oceanic whitetip shark (neonate, juvenile, and adult); smooth dogfish (all life stages); dusky shark (juvenile and adult); and sand tiger shark (juvenile and adult). 5.2.2 SOFT BOTTOM Surficial sediments of soft bottom substrate (consisting of unvegetated and unconsolidated sands) act as a storage bank for nutrients and chemicals, cycling between the sediments and the water column (Deaton et al. 2010). Soft bottom habitat is comprised of mud flats, beaches, shoals and sand bars. In the estuaries, soft bottom provides habitat for a variety of microscopic plants and benthic infaunal/epifaunal taxa. Together, these populations may serve as an important food source for many juvenile fish. Juvenile and adult fish species that forage on the abundance of microalgae, detritus, and small invertebrates in turn attract larger, economically valuable, predatory fish such as Florida pompano (Trachinotus carolinus), red drum (Sciaenops ocellatus), southern flounder (Paralichthys lethostigma), summer flounder (Paralichthys dentalus), spot (Leiostomusxanthurus), Atlantic croaker (Micropogonias undulatus), striped bass (Morone saxatilis), blue crab (Callinectes sapidus) and kingfisher (Menticirrhus spp). In the surf zone, inorganic nutrients are continually resuspended by wave action in sufficient concentrations to create localized phytoplankton blooms (Mclachlan et al. 1981; Hackney et al. 1996). This self-sustaining nutrient input perpetuates a cycle of phytoplankton production, which supports large numbers of intertidal filter feeders, high concentrations of baitfish and estuarine -dependent fish migrating through the surf zone including Florida pompano, gulf kingfish (Menticirrhus littoralis), summer flounder, southern flounder, red drum, and bluefish. Essential Fish Habitat Assessment — August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 24 According to Peterson and Peterson (1979), the most numerous meiofaunal taxon occurring in soft bottom habitats on subtidal and intertidal flats of North Carolina are the nematodes. Other meiofaunal taxa of these systems may include harpacticoid copepods, gastrotrichs, and turbellarians (Peterson and Peterson 1979). Investigations by Birkhead et al. (1979) indicated the abundance of polychaete worms in samples collected from the nearshore ocean at the mouth of the Cape Fear River. Representative polychaete worms included Spiophanes bombyx, Magelona sp., Heteromastus filiformis, and Paraprionospio pinnata. Additional taxa identified included the sea pansy (Renilla reniformis), the sand dollar (Mellita quinquiesperforata) and brittlestar (amphiurid). Relatively small, opportunistic species of polychaetes and amphipods tend to be the numerically dominant benthic macrofauna of intertidal and subtidal flats. Species abundances and diversity tend to decrease within higher intertidal areas and within areas of increased physical energy (e.g. on rapidly accreting shoals). Common macrobenthos of the oceanfront intertidal beaches include mole crabs, coquina clams, species of haustoriid amphipods, and certain polychaetes (e.g. Scolelepis squamata) (Deaton et al. 2010). Subtidal soft bottom offshore of Kure Beach was reported to be dominated by polychaetes with bivalves, crabs, and amphipods also prevalent (Posey and Alphin 2002). The marine soft bottom habitat of nearshore shoals provides important foraging habitat for several recreational and commercially important fish species that tend to congregate in or around areas of distinct topographic relief (Deaton et al. 2010). Both inlet shoals and cape -associated shoals are considered HAPC for managed species. Cape -associated shoals (such as FPS) generally extend from cuspate foreland promontories with sediment distribution influenced by wind -driven currents, waves, headland -related residual flows and tidal currents (McNinch unpublished). A report commissioned by BOEM (Rutecki et al. 2014) synthesized available data regarding ecological functions and the potential impacts from sand mining of shoals (the latter of which is described further in Section 5.0 below). The authors reported that while shoals and shoal complexes are among the least -studied marine habitats, there are sufficient data demonstrating their importance as refuge, forage areas, spawning sites, and nursery areas for a range of pelagic and demersal species. Shoal complexes (including inlet shoals and cape -associated shoals) have been designated EFH for a number of species including cobia, king mackerel, Spanish mackerel, red drum, and several Atlantic highly migratory species (Rutecki et al. 2014). FPS itself is identified as a HAPC for coastal migratory pelagics including the following managed species: cobia, king mackerel, and Spanish mackerel. FPS provides for benthic invertebrates adapted to dynamic substrate and serving as trophic base for demersal fish. It also serves as refuge for pelagic planktivores (e.g. anchovies, menhadens) that are prey species for resident and transient piscivores (e.g. bluefish, spiny dogfish, smooth dogfish, king mackerel, and Spanish mackerel). Subtidal bottom areas off the southeastern shoreline of North Carolina (including inlet shoals and cape - associated shoals) serve as pupping grounds for several species of shark including Atlantic sharpnose shark (Rhizoprionodon terraenovae), bonnethead shark (Sphyrna tiburo), blacknose shark (Carcharhinus acronotus), spinner shark (C. brevipinna), dusky shark (C. obscurus), and to a lesser degree, the blacktip shark (C. limbatus), sandbar shark (C. plumbeus), and scalloped hammerhead shark (S. lewini) (Deaton et al. 2010). The Magnuson -Stevens Act requires the identification of EFH in FMPs, and towards that end NMFS funded two cooperative survey programs designed to further delineate shark nursery habitats in the Atlantic and Gulf of Mexico. The Cooperative Atlantic States Shark Pupping and Nursery (COASTSPAN) Survey and the Gulf of Mexico States Shark Pupping and Nursery (GULFSPAN) Survey have been Essential Fish Habitat Assessment —August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 25 implemented to assess the geographical and seasonal extent of shark nursery habitat, determine which shark species use these areas, and gauge the relative importance of these coastal habitats in order to provide information that can then be used in EFH determinations. Limited COASTSPAN sampling occurred in nearshore waters along the southern coast of North Carolina from New River Inlet to the South Carolina border. Atlantic sharpnose was the most abundant species caught along with bonnethead, blacknose, blacktip and tiger sharks (NOAA 2009). 10' W,SM:/_\:i07:101fi101JL Hard bottom habitat in the South Atlantic Bight generally consists of exposed rock or consolidated sediments in nearshore or offshore marine waters. Exposed hard bottom provides the substrate surface area for colonization by invertebrates and algae as well as safe havens for larval and juvenile fish. In turn, these areas serve as an important food source to a variety of invertebrate and fish species. Community structure varies widely with depth, location, and season. Hard bottom habitats are characterized by a rich diversity of invertebrates (e.g. sponges, corals, anemones, tunicates, and mollusks) and reef fish such as gag grouper (Micteroperca microplepis), red grouper (Epinephelus morio), red snapper (Lutjanus campechanus), vermillion snapper (Rhomboplites aurorubens), black sea bass (Centropristis striata), greater amberjack (Seriola dumerili) and white grunt (Haemulon plumieri) and are thus commonly referred to as "live bottoms" or "live rock" (Deaton et al. 2010). The majority of hard bottom sites occur greater than three nautical miles from the shore. Other hard bottom sites may be subject to covering by storm -induced shifting sands and therefore may not be readily identified. According to the North Carolina Coastal Habitat Protection Plan (CHPP), northern Long Bay consists of a number of hard bottom sites occurring generally greater than one mile from shore. According to a report commissioned by the US Army Corps of Engineers (DCA 2010), there was no hard bottom habitat identified within the FPS borrow area considered for the Brunswick County Beaches Project based on the remote surveys and towed video confirmations performed at selected ground- truthing targets. Sediment samples confirm the presence of homogeneous sand throughout the FPS survey area. Similarly, the geotechnical investigation recently completed and documented by Olsen Associates (2016) did not reveal the presence of hard bottom within the proposed borrow site. 6. MANAGED SPECIES The SAFMC, Mid -Atlantic Fisheries Management Council (MAFMC), and Atlantic States Marine Fisheries Commission (ASMFC) have designated unvegetated bottom (hard and soft), and water column areas (estuarine and marine) within the study area as EFH, in compliance with the Magnuson -Stevens Fishery Conservation and Management Act (16 U.S.C. 1801-1882), as amended by the Sustainable Fisheries Act of 1996. Table 4 provides a list of all federally and state managed species (including life history stage) present in the Lower Cape Fear River, associated shoals, and estuary as identified by the NMFS. Species addressed in this section are representative and consist of fish and invertebrates of both recreational and commercial importance that are managed under the Magnuson -Stevens Fishery Conservation and Management Act and the 1997 Fisheries Reform Act which requires the North Carolina Division of Marine Fisheries (NCDMF) to prepare Fisheries Management Plans for review and adoption by the North Carolina Marine Fisheries Commission (NCMFC). The proposed action occurs in EFH categories (estuarine/marine water column and soft bottom) identified for several managed species including: brown shrimp (Farfantepenaeus aztecus), pink shrimp Essential Fish Habitat Assessment —August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 26 (Farfantepenaeus duorarum), and white shrimp (Litopenaeus setiferus); demersal species such as bluefish, summer flounder (Paralichthys dentalus), and red drum (Sciaenops ocellatus) ; coastal pelagics such as cobia (Rachycentron canadum), king mackerel, and Spanish mackerel; and various species of the snapper/grouper complex such as black sea bass (Centropristis striata), sheepshead (Archosargus probatocephalus), and gag grouper (Mycteroperca microlepis). Highly migratory species (HMS) with EFH in the vicinity of the proposed action include: longbill spearfish (Tetrapturus pfluegeri); blacktip shark (Carcharhinus limbatus), sandbar shark (Carcharhinus plumbeus), scalloped hammerhead shark (Sphyrna lewini), spinner shark (Carcharhinus brevipinna), tiger shark (Galeocerdo cuvier), blacknose shark (Carcharhinus acronotus), bonnethead shark (Sphyrna tiburo), and Atlantic sharpnose shark (Rhizoprionodon terraenovae). Other estuarine -dependent species including spot (Leiostomusxanthurus), Atlantic menhaden (erevoortia tyrannus), striped mullet (Mugil cephalus), blue crab (Callinectes sapidus), Atlantic croaker (Micropogonias undulates), kingfishes (Menticirrhus spp.), black drum (Pogonias cromis), and gray trout (Cynoscion regalis) that serve as prey for fisheries managed species (e.g. snappers, groupers, tuna, and sharks) inhabit the project area. Essential Fish Habitat Assessment — August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 27 Table 4. Presence of Managed Species (including life cycle stage) for Area Waterbodiesl [E=Eggs; L=Larval; J=Juvenile; A=Adult (A), N/A=Not Found] SPECIES Cape Fear River to US 421 Lockwoods Folly to NC 211 Myrtle Sound Masonboro Sound AIWW (throughout g NC) Atlantic Ocean South of Cape Hatteras Coastal Demersals Red drum ELJA ELJA ELJA ELJA ELJA A Bluefish ELJA ELJA ELJA ELJA ELJA JA Summer flounder LJA LJA LJA LJA LJA ELJA Invertebrates Brown shrimp ELJA ELJA ELJA ELJA ELJA ELJA Pink shrimp ELJA ELJA ELJA ELJA ELJA ELJA White shrimp ELJA ELJA ELJA ELJA ELJA ELJA Calico scallop N/A N/A N/A N/A N/A ELJA Snapper/Grouper Gag grouper J J J J J ELJA Gray snapper J J J J J ELJA Black sea bass LJA LJA LJA LJA LJA ELJA Gray triggerfish N/A N/A N/A N/A N/A ELJA Yellow jack N/A N/A N/A N/A N/A ELJA Blue runner N/A N/A N/A N/A N/A ELJA Crevalle jack N/A N/A N/A N/A N/A ELJA Bar jack N/A N/A N/A N/A N/A ELJA Greater amberjack N/A N/A N/A N/A N/A ELJA Almaco jack N/A N/A N/A N/A N/A ELJA Banded rudderfish N/A N/A N/A N/A N/A ELJA Spadefish N/A N/A N/A N/A N/A ELJA White grunt N/A N/A N/A N/A N/A ELJA Hogfish N/A N/A N/A N/A N/A ELJA Puddingwife N/A N/A N/A N/A N/A ELJA Essential Fish Habitat Assessment — August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 28 Table 4 (continued). Presence of Managed Species (including life cycle stage) for Area Waterbodies.1 SPECIES Cape Fear River to US 421 Lockwoods Folly to NC 211 Myrtle Sound Masonboro Sound AIWW (throughout g NC) Atlantic Ocean South of Cape Hatteras Blackfin snapper N/A N/A N/A N/A N/A ELJA Red snapper N/A N/A N/A N/A N/A ELJA Cubera snapper N/A N/A N/A N/A N/A ELJA Silk snapper N/A N/A N/A N/A N/A ELJA Vermillion snapper N/A N/A N/A N/A N/A ELJA Blueline tilefish N/A N/A N/A N/A N/A ELJA Sand tilefish N/A N/A N/A N/A N/A ELJA Bank sea bass N/A N/A N/A N/A N/A ELJA Rock sea bass N/A N/A N/A N/A N/A ELJA Graysby N/A N/A N/A N/A N/A ELJA Speckled hind N/A N/A N/A N/A N/A ELJA Yellowedge grouper N/A N/A N/A N/A N/A ELJA Coney N/A N/A N/A N/A N/A ELJA Red hind N/A N/A N/A N/A N/A ELJA Goliath Grouper (Jewfish) N/A N/A N/A N/A N/A ELJA Red grouper N/A N/A N/A N/A N/A ELJA Misty grouper N/A N/A N/A N/A N/A ELJA Warsaw grouper N/A N/A N/A N/A N/A ELJA Snowy grouper N/A N/A N/A N/A N/A ELJA Yellowmouth grouper N/A N/A N/A N/A N/A ELJA Scamp N/A N/A N/A N/A N/A ELJA Sheepshead N/A N/A N/A JA N/A ELJA Essential Fish Habitat Assessment — August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 29 Table 4 (continued). Presence of Managed Species (including life cycle stage) for Area Waterbodies.l SPECIES Cape Fear River to US 421 Lockwoods Folly to NC 211 Myrtle Sound Masonboro Sound AIWW (throughout g NC) Atlantic Ocean South of Cape Hatteras Red porgy N/A N/A N/A N/A N/A ELJA Longspine porgy N/A N/A N/A N/A N/A ELJA Scup N/A N/A N/A N/A N/A ELJA Coastal Pelagics Dolphin NA NA NA NA NA ELJA Cobia ELJA ELJA ELJA ELJA ELJA JA King mackerel JA JA JA JA JA ELJA Spanish mackerel JA JA JA JA LJA ELJA Highly Migratory Species Spiny dogfish JA JA JA JA JA ELJA Shortfin mako shark N/A N/A N/A N/A N/A N/A Blue shark N/A N/A N/A N/A N/A N/A Spinner shark N/A N/A N/A N/A N/A ELJA Scalloped hammerhead shark JA JA N/A N/A N/A JA Big nose shark JA JA N/A N/A N/A JA Black tip shark JA JA N/A N/A N/A JA Dusky shark JA JA N/A N/A N/A JA Night shark JA JA N/A N/A N/A JA Sandbar shark JA JA N/A N/A N/A JA Silky shark JA JA N/A N/A N/A JA Tiger shark JA JA N/A N/A N/A JA Atlantic sharpnose shark JA JA N/A N/A N/A JA Essential Fish Habitat Assessment — August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 30 Table 4 (continued). Presence of Managed Species (including life cycle stage) for Area Waterbodies.l SPECIES Cape Fear River to US 421 Lockwoods Folly to NC 211 Myrtle Sound Masonboro Sound AIWW (throughout g NC) Atlantic Ocean South of Cape Hatteras Longfin mako shark JA JA N/A N/A N/A JA Whitetip shark JA JA N/A N/A N/A JA Thrasher shark JA JA N/A N/A N/A JA Atlantic bigeye tuna N/A N/A N/A N/A N/A N/A Atlantic bluefin tuna N/A N/A N/A N/A N/A N/A Skipjack tuna N/A N/A N/A N/A N/A N/A Longbill spearfish N/A N/A N/A N/A N/A N/A Swordfish N/A N/A N/A N/A N/A ELJA White marlin N/A N/A N/A N/A N/A ELJA Sailfish N/A N/A N/A N/A N/A ELJA Yellowfin tuna N/A N/A N/A N/A N/A ELJA Blue marlin N/A N/A N/A N/A N/A ELJA Little tunny N/A N/A N/A N/A N/A ELJA 'Table contents from National Marine Fisheries Service (Beaufort, NC) 7. ASSESSMENT OF IMPACTS TO ESSENTIAL FISH HABITAT The following potential impacts to EFH are examined with regard to the Applicant's proposed action. Potential effects of the proposed action or actions on the EFH designations occurring within or adjacent to the project area are identified. Mitigative measures to be employed by the Applicant to reduce the potential adverse effects to EFH are included below. Potential consequences of the other viable project alternatives (as described in Section 2.4) are also summarized. Table 5 provides a summary assessment of the potential impacts to EFH and HAPC within or adjacent to the project area resulting from the implementation of the applicant's proposed action. The following assessment addresses those specific EFH categories occurring within or adjacent to the project area. These include: (1) estuarine and marine water column; and (2) soft bottom (including intertidal habitat of the surf zone and FPS, the latter of which is designated as HAPC). Essential Fish Habitat Assessment — August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 31 Table 5. Summary of Potential Impacts to Essential Fish Habitat and Habitat Areas of Particular Concern1,2 (N/A = Not Applicable; MAA = May Adversely Affect) ESSENTIAL FISH HABITAT Present w/in or adjacent to project area Impacts from excavation of borrow site Impacts from beach fill placement Estuarine Areas 1 Aquatic Beds NO N/A N/A 2 Estuarine Emergent Wetlands NO N/A N/A 3 Estuarine Scrub/Shrub Mangroves NO N/A N/A 4 Estuarine Water Column YES MAA MAA 5 Intertidal Flats YES NO NO 6 Oyster Reefs & Shell Banks NO N/A N/A 7 Palustrine Emergent & Forested Wetlands NO N/A N/A 8 Seagrass NO N/A N/A Marine Areas 9 Artificial/Manmade Reefs NO N/A N/A 10 Coral & Coral Reefs NO N/A N/A 11 Soft Bottom YES MAA MAA 12 Live/Hard Bottoms NO N/A N/A 13 Sargassum NO N/A N/A 14 Water Column YES MAA MAA GEOGRAPHICALLY DEFINED HABITAT Present w/in or Impacts from Impacts from adjacent to excavation of beach fill AREAS OF PARTICULAR CONCERN project area borrow site placement Area -Wide 14 Council -designated Artificial Reef Special NO N/A N/A Management Zones 15 Hermatypic (reef -forming) Coral Habitat & NO N/A N/A Reefs 16 Hard Bottoms NO N/A N/A 17 Hoyt Hills NO N/A N/A Essential Fish Habitat Assessment — August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 32 18 Sargassum Habitat NO N/A N/A 19 State -designated Areas Important for Managed Species NO N/A N/A 20 Submerged Aquatic Vegetation NO N/A N/A North Carolina 21 Big Rock NO N/A N/A 22 Bogue Sound NO N/A N/A 23 Coastal Inlets YES NO NO 24 Capes Fear, Lookout & Hatteras (sandy shoals) YES MAA MAA 25 New River NO N/A N/A 26 The Ten Fathom Ledge NO N/A N/A 27 The Point NO N/A N/A 'As identified in the Fishery Management Plan Amendments of the South Atlantic Fishery Management Council zAdapted from USACE Environmental Assessment - Preconstruction Modifications of Authorized Improvements, Wilmington Harbor, North Carolina (February 2000) 7.1 ESTUARINE AND MARINE WATER COLUMN During the dredging process and sand placement for beach nourishment, immediate localized impact originating from removal of substrate and the abrupt increased sedimentation of the marine water column at both the borrow sites and intertidal surf zones adjacent to the construction area and disposal sites are expected. Localized increases in turbidity also has the potential to reduce benthic prey availability (Deaton el al. 2010). According to USACE (1997), sediment consisting of more than 90% sand is not likely to produce significant long-term suspension of sediment or turbidity and any effects of elevated turbidity levels tended be limited both temporally and spatially. Turbidity levels decrease rapidly subsequent to dredging and disposal through simple mixing and dilution processes (associated with longshore and tidal currents, wind, and surf). Indeed, storm events can produce equally high levels of suspended sediments. The sandy substrate of both the borrow site and the nourishment site will reduce the potential for any significant or prolonged elevation of turbidity levels in the water column. Larval/early juvenile fish species spawned in the offshore and nearshore waters arrive in the inlets of North Carolina in three distinct stages: winter -early spring, late spring, and summer with the peak abundance occurring in late spring (Hettler and Chester 1990). Seasonal restrictions on dredging for navigation projects has been shown to be an effective means of protecting fish during critical life stages, such as spawning or juvenile fish growing periods in nursery areas (NCDEQ 2016). Hydrodynamic modeling performed by Olsen for the project EIS (2014) predicted that there is no inlet - directed tidal flow on either peak ebb or peak flood conditions at Frying Pan Shoals. Therefore, there is no expected effect on the entrainment of larvae from the proposed borrow site by tidal action. Given the Essential Fish Habitat Assessment —August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 33 size of the proposed borrow site relative to the large shoal feature (less than 0.5%) and the predicted physical recovery of the borrow area, it can be reasonably expected that the proposed action will not induce any large-scale disruption to circulation patterns. In addition, the excavated area will tie into natural bottom contours on the western edge of the shoal feature (i.e. there will not be a hole that could theoretically entrap or slow larvae). Rather, it is likely that vertical mixing and upwelling patterns would continue to be maintained with only limited, localized effects to currents/circulation. As a result, there is not expected to be an effect on the transport of larvae. Lastly, any assumed impacts to circulation (or disruption to upwelling) is unlikely to affect larval transport given that larvae have been demonstrated to exert considerable control over vertical movement within the water column (Morgan and Anastasia, 2008). Migration of larvae outside the tidal influence of the estuary is influenced through wind -driven transport and directed vertical movement by larvae to maximize shoreward movement (Boehlert and Mundy, 1988). Once nearshore, then alongshore drift is the principal mechanism until larvae reach the entrainment influence of the estuary. Based upon the lack of pronounced effects to circulation patterns, the uninterrupted wind -driven transport of larvae, the ability of larvae to exert control over vertical movement, and the large entrainment field of the Cape Fear River estuary; larval transport into the estuary will not be adversely affected. Although limited data are available regarding impacts of beach nourishment on transient or resident surf zone fishes (especially early life history stages), it is anticipated that performing the work during periods of reduced biological activity will reduce potential adverse impacts to these life history stages. Research conducted by Ross and Lancaster (1996) focused on the use of the surf zone by two species, Florida pompano (Trachinotus carolinus) and Gulf kingfish (Mentecirrhus littoralis), as a nursery. Both species were reported to exhibit a high degree of site fidelity. Placement of beach fill within the surf zone would likely have a temporary impact upon these fish through the burial of their primary forage of amphipods and coquina clams (Donax variabilis). Recolonization and species recovery of these affected areas of the surf zone by benthic prey species is generally rapid when the deposited material is compatible with that of the beach front where it is to be placed. Studies conducted on the changes in geomorphology and sediment characteristics indicate that these factors have a greater impact upon benthic recovery than the actual burial (USFWS 2000). Given the proposed length of shoreline to be nourished, a relatively small percentage of these larval/early juvenile fishes would be affected. Also, considering the compatibility of the material to be deposited with the existing beach sediments, relatively quick recovery of the benthic fauna through horizontal and vertical migration is expected. A study conducted by Versar, Inc. (Versar 2004), on behalf of the USACE Wilmington District, collected data over a two year period on the "Effects of Dredge Material Beach Disposal on Surf Zone Fish and Benthic Resources on Bald Head Island, Caswell Beach, Oak Island, and Holden Beach, North Carolina, 2003 and 2004". During the years 2001-2002, the USACE Wilmington Harbor Project deepened and realigned the entrance channel to the Cape Fear River. Approximately 5.6 million cubic yards of material was removed from the Cape Fear River navigation channel as well as the offshore navigation channel leading to the river entrance. This material was then deposited on the four mentioned beaches to replenish areas affected by erosion over the previous years. Dredging and sand placement occurred between Spring 2001 through Winter 2002. Following both year 1 and year 2 sampling, Versar reported that no immediate impacts in fish abundances and diversities among disturbed, undisturbed, and reference stations were identified at any of the four beaches. Essential Fish Habitat Assessment — August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 34 Increased turbidity associated with beachfront disposal is minimized through dewatering of material behind upland dikes. The nature of the material dredged (i.e. less than 2% fines) will serve to minimize turbidity problems. In general, the spatial scale of elevated turbidity related to dredging and beachfront disposal is very small (USACE 2001). In addition, the area of shoreline for the proposed nourishment has been the location for prior federal sand disposal associated with maintenance of the adjacent Wilmington Harbor Entrance Channel. The proposed nourishment limits of the Village -sponsored project are consistent with the authorized federal disposal project. Mortality of organisms (i.e. pelagic eggs and larvae to pre -flexion stage individuals) within the water column that lack the ability to escape the suction field of an operating dredge and subsequent entrainment in the flow of water and sediment passing through its pumping equipment is likely. However, previous USACE studies have demonstrated that only an extremely small percentage (a fraction of 1%) of marine and estuarine water column inhabitants are subject to entrainment based upon the amount of water that a dredge can pump. In similar soft bottom habitats, Van Dolah et al. (1992) estimated that mortality of post larval shrimp (L. setiferus) due to entrainment during dredging activities was in the order of 1,883 individuals. This was considered insignificant since a single female white shrimp produces between 500,000 and 1,000,000 eggs each spawning period. Impacts to sessile, slow moving taxa that cannot escape the suction field of the dredge are expected but limited. Due to the mobile nature of most fish assemblages it is believed that these fish will relocate to other areas while dredging activities take place. Subsequently, effects on these life forms are expected to be relatively minor relative to local or regional population levels. Pullen and Naqvi (1983) found that motile animals were the least affected by dredging and concluded that benthic and fish utilization likely depends upon water quality of the dredge area. Provided the dredge area does not form an anaerobic pit of organic -laden sediment, biological communities may be restored rather quickly. In addition, multiple studies have indicated rapid recovery of benthic populations and fish utilization at locations with high water and sediment dynamics such as tidal channels (Pullen and Naqvi 1983; Van Der Veer et al. 1985; Schaffner et al. 1996; Musick 1998). The proposed action may adversely affect the estuarine and marine water column EFH (including managed species utilizing these habitats); however, potential adverse effects due to the following considerations: (1) limited spatial and temporal effects of elevated turbidity (due to high quality and compatibility of sand material); (2) avoidance behavior and mobility of finfish; (3) the small fraction of water column to be affected by the proposed activities (relative to the volume of water in the nearshore waters of the Cape Fear River and nearby beaches; and (4) the timing of the proposed action start date coinciding with decreased water temperatures and decline in fish abundances. 7.2 SOFT BOTTOM Soft bottom consists of unconsolidated, unvegetated sediment of freshwater, estuarine, and marine systems (Street et al. 2005). For the purpose of this EFH Assessment, soft bottom is principally associated with the marine intertidal beach and the shallow subtidal bottom of the surf zone (at the nourishment site) and the marine sandy, subtidal bottom of FPS. Note the nourishment site of West Beach is located along the estuarine shoreline adjacent to the federal Wilmington Harbor Entrance Channel. Each of the soft bottom categories are characterized as high energy environments with high percentage sand content (and correspondingly low percent fine-grained sediments and low percent organic content). High water velocities and shifting sand shoals within higher energy areas (e.g. surf zone and depositional shoals) Essential Fish Habitat Assessment —August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 35 present a largely prohibitive environment for most bottom -dwellers (Posey et al. 1996). Benthic assemblages of depositional, sandy shoals are opportunistic in nature and tend to be adapted to disturbance -prone environments. 7.2.1 SURF ZONE Implementation of best management practices associated with more recent beach nourishment helps to reduce potential adverse effects to soft bottom habitat and the managed species that utilize these areas for foraging. Use of high quality, beach compatible sand generally limits the spatial and temporal extent of elevated turbidity levels while promoting more rapid recovery of benthic fauna of the supratidal beach and swash zone. In addition, the nourishment will be performed during periods of reduced biological activity. While certain fish species may be displaced for a short period during the pumping of material onto the beachfront, some demersal species may be attracted to this type of disturbance due to the suspension of prey items in the water column (CZR and CSE 2015). Impacts to the soft bottom of the surf zone will occur through burial and mortality of benthic fauna. However, these effects are generally considered short-lived and are of a scale that is not expected to result in any pronounced impact to the EFH or to the species utilizing this type of habitat. Consideration should also be given to the maintenance of a wide upper beach resulting in benefits to the intertidal habitat in comparison to alternatives such as hardened structures (NCDEQ 2016). 7.2.2 FRYING PAN SHOALS The proposed sand source site is located on the western flank of FPS approximately 1 mile southeast of the South Beach shoreline. The shoals extend approximately 32 miles offshore of Bald Head Island. FPS is a highly dynamic and renewable shoal feature maintained by seaward flow of the currents off the cape. As described previously, FPS is identified as a HAPC for coastal migratory pelagics including the following managed species: cobia, king mackerel, and Spanish mackerel. FPS provides for benthic invertebrates adapted to dynamic substrate and serving as trophic base for demersal fish. It also serves as refuge for pelagic planktivores (e.g. anchovies, menhadens) that are prey species for resident and transient piscivores (e.g. bluefish, spiny dogfish, smooth dogfish, king mackerel, and Spanish mackerel). Subtidal bottom areas off the southeastern shoreline of North Carolina (including inlet shoals and cape -associated shoals) serve as pupping grounds for several species of shark (Deaton et al. 2010). There are limited number of field studies examining the impacts of sand mining on individual fish or fish populations (Michel 2013). Available literature summarizing potential adverse effects of offshore borrow sites commonly address concerns with respect to the following general impact categories: (1) elevated turbidity levels; (2) reduction in prey availability for foraging fish species; (3) long-term alteration of habitat from the physical removal of sand (including the potential disruption of wave climate influencing physical recovery); and (4) potential effects to hard bottom habitat underlying shallow sand deposits. These general impact categories in the context of the proposed action are discussed further below. Note that turbidity effects have been evaluated in Section 7.1 above. In addition, Section 3 above identifies SAFMC protection measures for dredging within identified HAPCs and avoidance and minimization measures specific to the proposed action. Prey Availability.- Subtidal shoals tend to be rigorous environments for marine organisms with physical stressors affecting benthic populations (Peterson and Peterson 1979). The faunal community is a function of the substrate and energy regime of the area and varies naturally through time in response to physical changes (Hobbs 2002). Given that these soft bottom areas are regularly affected by shifting sands, the Essential Fish Habitat Assessment —August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 36 dominant taxa are opportunistic in nature and thus are adapted to relatively rapid colonization and recovery (Posey and Alphin 2001). Benthic regeneration of a disturbed area will vary depending upon the magnitude of the disturbance, the character of the new sediment interface, duration and timing of the dredging, the type of equipment used to extract the sediment, life history characteristics of colonizing species, water quality, and rate of sediment recovery (Pullen and Naqvi 1983; Van Dolah et al. 1992). Faunal recovery may take more time if the excavation significantly alters the character of the sediment interface or if poor water quality ensues due to low wave energy and high organic matter. Though species abundances may return to pre -dredging conditions rather quickly, species composition and diversity indices may remain altered for a period of time subsequent to excavation (Jutte and Van Dolah 1999). However, benthic infaunal populations recover rather quickly provided that the post -dredging environment is favorable for colonization (i.e. dynamic, accreting sandy shoals with low percent organic content) (Bergquist et al. 2008) and that peak periods of larval recruitment are avoided (National Research Council 1995; Hackney et al. 1996). While removal of sediments during dredging results in direct mortality to benthic infauna, several studies have indicated relatively rapid recolonization and species recovery of benthos subsequent to dredging operations (Pullen and Navqi 1983; National Research Council 1995; Hackney et al. 1996; Schaffner et al. 1996). Posey and Alphin (2002) concluded that the rapid infilling of a borrow site (resulting from strong water currents and dynamic sand movement) contributed to a relatively quick species recovery. Based upon the results of this study, interannual variability contributed more to the observed differences in species abundance than the sediment removal effects (Posey and Alphin 2002). Saloman et al. (1982) concluded that faunal abundance of a dredge site recovered within three months subsequent to dredging. The authors also determined that species diversity and faunal composition had returned to pre -dredge conditions within nine months. The Town of Nags Head completed a beach nourishment project in 2011 that placed 4.71Mcy from an offshore shoal borrow site along approximately 10 miles of shoreline. In the first post -project year benthic monitoring (CSE, 2012), results for the winter/winter and spring/spring samples showed no significant difference in richness between pre- and post -nourishment samples at the borrow site. However, winter/spring numbers were measurably different in both the pre- and post- samples at both the control site and borrow site. These data indicated that seasonal differences were greater than differences between the control and impact sites. Benthic monitoring associated with prior Bald Head Island nourishment projects has demonstrated rapid recolonization of dredged sites by characteristic taxa. For the Village -sponsored beach nourishment project constructed in the winter of 2009/2010, benthic monitoring was conducted pre -dredge and post - dredge (for three years) in both reference shoals (Middle Ground and Bald Head Shoals) as well as in the authorized borrow area of Jay Bird Shoals. Monitoring indicated that mean total abundances did not differ between years at any of the sites (Jay Bird Shoals, Bald Head Shoals, and Middle Ground) sampled. In 2012 (Year 3 post -dredging), mean total abundance at Jay Bird Shoals was greater than at two of the three reference sites (Middle Ground and Jay Bird Reference), but the differences were not significant. Similar to the reference sites, diversity and species richness at Jay Bird Shoals did not significantly differ between 2009 (pre -construction) and 2012 (post -construction Year 3). The infaunal assemblage at Jay Bird Shoals was dominated by amphipods and other taxa which are adapted for life in environments prone to natural disturbance. These taxa presumably recolonized quickly after project construction and were joined by Essential Fish Habitat Assessment — August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 37 other taxa that may have capitalized on the reduced competition for space associated with recently disturbed habitats. The rapid recolonization of Jay Bird Shoals observed in 2010 (Year 1 post -construction) appeared to have resulted in a relatively stable benthic community assemblage which persisted through 2011 and 2012 (LMG 2013). Dominance patterns were also similar between years at the Jay Bird Shoals borrow site. In all four years, Jay Bird Shoals was dominated by the amphipod Protohaustorius wigleyi. The gastropod Olivella mutica was also dominant at this site in all four years. Although there were some species that were dominant at Jay Bird Shoals during one year but not the other years, this appears to reflect natural interannual variability which is typical of benthic infaunal communities, particularly in high-energy environments susceptible to periodic natural disturbance. Similar to the reference sites, diversity and species richness at Jay Bird Shoals did not significantly differ between 2009 (pre -construction) and 2012 (post -construction Year 3). The third and final year of post -construction data indicated that the benthic community inhabiting the Jay Bird Shoals borrow site recovered quickly from any potential deleterious effects of project activities and that the recovery was persistent. Benthic monitoring was also conducted in association with the Village's Bald Head Creek dredge and nourishment project in 2012. Benthic infaunal sampling of both reference shoals and dredged shoals (pre - and post -dredging) indicated that dominance patterns remained relatively stable between years. Polychaetes and amphipods were among the most abundant taxa collected at both sites during all years (pre- and post -construction). Six taxa were dominant at one or both sites during all four sampling years (Acanthohaustorius intermedius, Caulleriella venefica, Nematoda sp., Paraonis fulgens, Protohaustorius cf. wigleyi, and Spiophanes bombyx). At the borrow site, many of the same species that were dominant in pre -construction sampling were also dominant in post -construction Year 3 sampling. Amphipods of the family Haustoridae (Acanthohaustorius intermedius and Protohaustorius cf. wigleyi) have been documented to colonize quickly after disturbances (Levinton 1982, Posey and Alphin 2002). These organisms may be especially adapted for life in disturbance -prone environs of depositional, sandy shoals as their ability to multiply rapidly once established makes them resilient to environmental perturbations. The dominance of relatively opportunistic species such as these likely contributed to the rapid recovery of the Bald Head Creek Shoal borrow site observed in Year 1, the recruitment pulse observed in Year 2, and the continued robustness of the benthic community documented in Year 3. Polychaetes were also dominant taxa at the Bald Head Creek Shoal borrow site during all four years of sampling. Most polychaetes are considered to be good dispersers, and many have planktonic larvae. The mobility of these dominant polychaetes inhabiting the borrow site likely contributed to the resilience of the benthic community observed during the four years of sampling. The third and final year of post -construction monitoring (2015) indicated that the benthic communities inhabiting the Bald Head Creek Shoal reference and dredge sites are resilient. Diversity, species richness, and mean total abundance at the borrow site were significantly higher during Year 3 post -construction sampling than during Year 0 pre -construction sampling. Diversity, richness, and mean total abundance were all significantly greater at the borrow site than at the reference site during Year 3 monitoring. Based upon pre- and post -construction monitoring, there was no discernible adverse effect on benthic populations resulting from project dredging. In fact, these resilient benthic communities may actually Essential Fish Habitat Assessment —August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 38 thrive in environments that are prone to disturbance. Factors contributing to the recovery and robustness of the benthic community at the Bald Head Creek Shoal borrow site included: (1) the consistency of sediment texture/composition both pre- and post -dredging; (2) the presence of undisturbed shallow subtidal bottom that can serve as a source for recruitment into the dredged area; and (3) the opportunistic and resilient nature of the benthic taxa inhabiting the disturbance -prone shoal habitat (LMG 2015). High densities and fecundity of infaunal species would minimize any potential long-term adverse effects on benthos. The proposed FPS dredge site is depositional in nature and thus subject to rather rapid infilling, sediment recovery, and benthic infaunal recruitment. The location of the borrow site precludes the deposition of fine, organic -laden sediments. Changes in sediment character and resultant anoxic/hypoxic conditions are cited as principle causal factors restricting benthic re -population (NRC 1995). Additionally, timing of the dredging is important in light of peak recruitment periods and adult activity. Avoiding these peak periods of biological activity (i.e. dredging fall through winter) will facilitate post -dredging recovery since larval recruitment and adult migration are the primary recolonization mechanisms (Herbich 1992). HabitatAlteration and Effects on Species Utilization. -Vertical relief associated with FPS (as with other shoal habitats) provides refuge for numerous species (e.g. anchovies, menhaden) that are prey species for resident and transient piscivores (e.g. bluefish, spiny dogfish, smooth dogfish, king mackerel, and Spanish mackerel). Offshore shoals or cape -associated shoals represent multi -use habitat for several species and potential spawning areas for demersal species and schooling planktivores (CSA International, Inc. 2010). Study of a federal dredging project at Asbury Park/Manasquan Inlet, New Jersey found that fish species assemblages and abundances post -dredging were similar to that of a previous study of the area. In addition, the researchers concluded that feeding habits of winter flounder and summer flounder remain unaltered post -dredging (USACE 2001). Van Dolah et al. (1994) found that changes in species composition between pre- and post -dredging monitoring were attributed to normal seasonal and yearly variability rather than from the effects of dredging. Van Dolah et al. (1992) evaluated effects of dredging on recreationally important fish species based upon changes in the abundance of prey species. Findings of this particular study indicated that there were no appreciable differences subsequent to dredging. Other studies have actually demonstrated an increase in fish utilization subsequent to dredging. Fish may be attracted to a dredged area due to suspended nutrients and infauna in the water column and as a haven from cold surface water in the winter (Courtenay et al. 1980; Pullen and Naqvi 1983). Schaffner et al. (1996) concluded that a dredged borrow area in the lower Chesapeake Bay provided more favorable habitat for the blue crab. No changes in the within -sediment depth distributions of macrobenthos (an indication of availability to fish and crustacean predators) were observed subsequent to dredging. The authors concluded that it was "unlikely that the resource value of benthos in trophic support of fisheries was negatively impacted" (Schaffner et al. 1996). Demersal grazers and detritivores will be able to move and forage upon expansive subtidal bottom available adjacent to the project area while infauna and macrofauana recover. Given the mobility of these species and small area of excavation proposed compared to the expansive shallow subtidal habitat of the larger FPS feature, the proposed action is not anticipated to have widespread effects upon the larval and juvenile life history stages of prey species utilizing the project area. Using a conservative estimate of the aerial extent of the most prominent shoal feature, there is approximately 42,000 acres of shallow soft bottom habitat of which the proposed dredge area consists of 188.7 acres, equivalent to 0.45% of the Essential Fish Habitat Assessment — August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 39 aerial extent of FPS. Subsequent to the dredging, post -construction monitoring will evaluate both physical and biological (benthic infaunal) recovery. Prior to any future use of the site, the findings of the post - construction monitoring will be reviewed by resource and permitting agencies for use in any future permit decisions. In addition, the Applicant will prioritize the use of Jay Bird Shoals as a borrow site prior to future use of the FPS borrow site. It is expected that demersal species will relocate to other expansive areas of unaffected soft bottom habitat on, and adjacent to, the shoal during the period of construction activities and subsequent benthic recovery period. Finfish will return to the project area within a short period of time taking the opportunity to forage upon suspended nutrients and benthic infauna. Subsequently, the potential adverse effect on fisheries resources dependent upon soft bottom habitats is expected to be relatively minor. While knowledge of the geology and ecological importance of shoals is incomplete and additional research is needed to improve the understanding of the mechanism for maintenance of shoals (Hayes et al. 2004, Michel 2013, Rutecki et al. 2015), the long-term alteration of habitat is minimized based upon the size and siting of the borrow site within such a large, dynamic and depositional feature. As discussed above, only 0.45% of the shallow soft bottom habitat associated with FPS is proposed for dredging. The proposed volume of 2.5 Mcyrepresents 0.18% of the estimated 1.46cy total volume of sand within FPS. Sediment input from updrift cuspate forelands provides active recharge of the shoal feature. The position of the borrow site on the western flank will allow for more rapid physical recovery. According to McNinch (unpublished), the crest of the shoal is "likely planed -off during storm conditions, when waves are steep and breaking across the shoal". Sediment during these events is transferred to the flanks of the shoal. The combination of the size and position of sand source site (on the western flank) minimizes effects to the shoal integrity and will have minimal influence on processes contributing to shoal formation and maintenance. As a result, the overall morphology of the cape -associated shoal will remain unchanged. With respect to the predicted rate of sediment transport, McNinch (2009) observed the following: "The most active region of sediment recharge to FPS is likely near the cape point, particularly along the crest of the shoal where it extends seaward from the subaerial cape point and the shore parallel sand bar that merges into FPS from the updrift beach". (Note — the updrift beach or shoreline northward of the cape point is known as East Beach on BHI). Numerous individuals or organizations have performed estimates of littoral transport along the ever - varying shoreline components of the State of N.C. More recently, (Van Gaalen, Tebbens and Barton, 2016) have summarized sediment transport directions from Northern Maine to Tampa Bay, FL. For the Cape Fear formation, the published rates for the two Bald Head Island shorelines that join to form the Cape Fear Point are as follows: • South Beach — 339,300 cubic meters annually toward the East. • East Beach — 341,000 cubic meters annually southward. This represents a potential net annual hypothetical rate of deposition to the Cape Fear Shoal formation of 680,300 cubic meters (i.e. 813,215 cy). Annual monitoring of South Beach indicates that net easterly transport would typically be less than that estimated above. Essential Fish Habitat Assessment —August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 40 Given the size of the proposed borrow site relative to the large shoal feature (less than 0.5%) and the predicted physical recovery of the borrow area, it can be reasonably expected that the proposed action will not induce any large-scale disruption to circulation patterns or to larval transport to the shoreline and to the Cape Fear River estuary. In addition, the excavated area will tie into natural bottom contours on the western edge of the shoal feature (i.e. there will not be a hole that could theoretically entrap or slow larvae). Rather, it is likely that vertical mixing and upwelling patterns would continue to be maintained with only limited, localized effects to currents/circulation. As a result, there is not expected to be an effect on the transport of larvae. Lastly, any assumed impacts to circulation (or disruption to upwelling) is unlikely to affect larval transport given that larvae have been demonstrated to exert considerable control over vertical movement within the water column (Morgan and Anastasia, 2008). Larvae and early juveniles are not passive in their movement. Migration of larvae outside the tidal influence of the estuary is influenced through wind -driven transport and directed vertical movement by larvae to maximize shoreward movement (Boehlert and Mundy,1988). Once nearshore, then alongshore drift is the principal mechanism until larvae reach the entrainment influence of the estuary. Larvae are adapted to highly dynamic physical conditions in nearshore environments. Based upon the lack of any significant effects to circulation patterns, the uninterrupted wind -driven transport of larvae, the ability of larvae to exert control over vertical movement, and the large entrainment field of the Cape Fear River estuary; larval transport into the estuary will not be adversely affected. A number of factors help to minimize the effects of the proposed alternative to this category of EFH within or adjacent to the proposed project area. These include: (1) the mobility of finfish and associated avoidance behavior; (2) selection of the borrow site to maximize suitable post -dredging sand quality and consistency; (3) the physical conditions of the dredge site favoring rapid infilling and benthic recovery; (4) the presence of undisturbed, exclusion zones serving as refuge patches and sources of colonization for benthic infauna; (5) avoidance of peak benthic and larval fish recruitment periods; and (6) fecundity and opportunistic nature of benthic communities of this type of habitat. In order to quantify and monitor the infilling of the borrow and surround shoal effects, monitoring will be conducted as described in Section 4 above. 7.3 HARD BOTTOM There are no known hard bottoms occurring in the vicinity of the proposed borrow area(s) to be dredged (Rester et al. 2001, DCA 2010). For projects occurring in the vicinity of hard bottom areas, excavation of soft bottom and subsequent changes to shoaling patterns can potentially result in secondary effects to these communities. Hard bottoms may become covered by thin layers of sand (as is more often observed through storm -induced shoaling). Given the lack of observed hard bottoms near the project area, it is anticipated that excavation activities from the source site and subsequent sand placement on West Beach and South Beach will not adversely affect hard bottoms or their associated fish assemblages in the nearshore or offshore waters off Bald Head Island. 8. IMPACT SUMMARY FOR ESSENTIAL FISH HABITAT The functional value of the lower Cape Fear River and its associated sandy shoals serve as a conduit between the open ocean environment and the estuarine environment for passage of larval, juvenile, and adult fish species as well as organisms of lower trophic levels (e.g. phytoplankton and zooplankton) and is an essential component of fishery habitat. While certain EFH categories will be subject to short-term Essential Fish Habitat Assessment —August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 41 impacts, these disturbances are considered temporary and localized. The potential effects on managed fish and essential fish habitat from the proposed action include: • Temporary loss of foraging habitat and prey availability through burial at the nourishment site; • Temporary suspension of sediments at the excavation site and nourishment site (i.e. surf zone) which could affect foraging; • Entrainment and mortality of benthic infaunal species during dredging; and • Longer -term habitat alteration of the borrow site. The proposed action is not anticipated to have any long-term effects on EFH and managed species. This is due in part to the following considerations: (1) the limited spatial and temporal effects of elevated turbidity due to high sand content of dredged sediments and rapid dilution; (2) the mobility of finfish and associated avoidance behavior; (3) the physical conditions of the dredge site favoring rapid infilling and benthic recovery; (4) avoidance of peak benthic and larval fish recruitment periods during dredging and nourishment; (5) fecundity and opportunistic nature of benthic communities to accommodate anthropogenic and natural disturbance; and (6) the avoidance and minimization measures described in Section 3 above. Sand source sites of high volume, beach compatible sand are limited (Section 2.4). Sites that may yield large volumes of beach compatible sand may be operationally prohibitive or cost -prohibitive if they are located too far from the nourishment site. As indicated previously, Jay Bird Shoals (JBS) has demonstrated to be a viable sand source site for the Village. It should be noted that JBS is a more finite resource and is identified as HAPC for shrimp, estuarine -dependent snapper -grouper, and red drum by the SAFMC. Moreover, in consideration of the recently constructed Village -sponsored nourishment project (2018/2019) and the recently authorized Town of Oak Island project, use of JBS as a potential sand source site is not viable for the foreseeable future. Additional removal of material from JBS under the current and anticipated near -term conditions would provide temporary benefits at best with the likelihood of reducing beneficial effects in their lee on one or both of the two adjacent barrier islands. Hence, "over - utilization" of these potential sand sources is not recommended and, in all probability, would be strongly opposed by interests on the east end of Oak Island. However, the borrow site previously permitted for Village -sponsored projects is continuing to be physically monitored on an annual basis. If the shoreline of South Beach can be maintained though federal nourishment for a period of time and sufficient physical recovery occurs within JBS prior to the next nourishment need, then the Village will seek to utilize JBS as an alternative sand source site prior to the use of FPS. Physical monitoring of the JBS borrow site will determine the volume of sand available for dredging prior to the next Village -sponsored nourishment, and this information will be provided to the agencies to determine if JBS can be utilized in lieu of FPS. Given the size of the proposed borrow area relative to the FPS feature (both spatially and volumetrically) and the annual rates of sediment input, the morphological integrity of the shoal will not be affected by the proposed action. Provided the overall physical integrity of the shoals is maintained, then potential adverse effects to ecological functions are minimized. In general, it is preferable to utilize sites that are anticipated to have a high likelihood of physical and biological recovery. The location of the borrow site Essential Fish Habitat Assessment —August 2020 Village of Bald Head Island FPS Beach Nourishment Project Brunswick County, North Carolina 42 on the western flank of FPS ensures infilling with sand (consistent with the existing substrate) and a relatively high rate of recharge. In light of the favorable physical conditions of the borrow site (suitable substrate and characteristics favorable for physical and biological recovery), avoidance of other sensitive EFH habitats, adherence to the identified SAFMC protection measures, and incorporation of additional mitigative actions, it is believed that potential adverse effects to EFH and managed species are minimized. 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SOUTH BEACH RENOURISHMENT PROJECT DRAWN BY: 2618 Herschel Street ML - �� Jacksonville, FL.32204 (904) 387-6114 FRYING PAN SHOALS SHEET • C-1468 BORROW SITE DETAILS 7 of 9 ELEVATION (FT, NAVD88) Q Ln + O LO 0 N N M 0)W L~L N Z Z F LLLL LLLL w N N Q w H 2 O O O Q Q a 0L D w � o U) J W 77 m 0 Q _ O w IL J W m \ p Q o o z � Lrio" C9 O w W J a ❑ _ r) ~ ILL N 0 fY 0 0 w w Q m , W ILL Q w () z ~ z z O w I= m Ln C) 0 0 W Q o u) M \ o 0 N / 00 z O Lu Cw7 0 o w LL J v H � � O IIIql _ � O O Q}+ N O W W i-y .+. N ❑ N _ CO 3 w 0 c=g>>�g z Zz z O J Q F71 I I I I I I I I I I I I I lJ J Ln O + IA C. In O Ln 7 7 N N lM O (89GAVN '13) NOIIVA313 NOT FOR PURPOSES OF CONSTRUCTION Olsen VILLAGE OF BALD HEAD ISLAND DATE APPROVED REVISION 07/01/2019 associates, inc. SOUTH BEACH RENOURISHMENT PROJECT DRAWN BY: ma G 2618 Herschel Street ML Jacksonville, FL. 32204 FRYING PAN SHOALS SHEET (904) 387-6114 C-1468 BORROW SITE SECTION A -A' 8 of 9 olsen associates, inc. 2618 Herschel Street Jacksonville, FL. 32204 (904)387-6114 C-1468 VILLAGE OF BALD HEAD ISLAND SOUTH BEACH RENOURISHMENT PROJECT FRYING PAN SHOALS BORROW SITE CULTURAL RESOURCES EXCLUSION ZONE NOT FOR PURPOSES OF CONSTRUCTION DATE I APPROVED I REVISION 07/01/2019 DRAWN BY: ML SHEET 9 of 9