HomeMy WebLinkAbout3_06010203 Tuckasegee20
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WateRsHeD at a gLance
counties:PoPuLation:2006 LanD coveR:PeRmitteD FaciLities:
Jackson, Swain 2000: 41,737 Open Water.............1%NPDES
municiPaLities:2010: 49,162 Developed...............5% Wastewater Discharge........22
Bryson City, Dillsboro, Forest Hills, Sylva, Webster Forested.................89% Wastewater Nondischarge....8
ePa LeveL iv ecoRegions:aRea 734 mi2 Scrub......................1% Stormwater..........................16
High Mtns., Southern Metasedimentary Mtns,
Southern Crystalline Ridges & Mtns Agriculture...... ........4%Animal Operations...................0
Figure 1-1: NLCD 2006 LaND Cover
Ü
2006 Land Cover
Water
Developed, Open Space
Developed, Low Intensity
Developed, Medium Intensity
Developed, High Intensity
Barren Land
Deciduous Forest
Evergreen Forest
Mixed Forest
Shrub/Scrub
Grassland
Pasture/Hay
Cultivated Agriculture
Woody Wetlands
tuckasegee RiveR
subbasin
HUC 06010203
Includes: Tuckasegee River, Caney Fork, Scott Creek,
Savannah Creek & Oconaluftee River
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Figure 1-2: TuCkasegee river subbasiN Map (06010203)"à)
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SWAIN
MACON
JACKSON
HAYWOOD
CLAY
GRAHAM
CHEROKEE
TRANSYLVANIA
TENNESSEE
Highlands
Sylva
Franklin
Bryson
City
WebsterRobbinsville
ForestHills
Dillsboro
Santeetlah
S c o t t C r eek
R
a
v
e
n For
k
Snowbird Creek
Nantah
a
l
a
R
i
v
e
r
Cheoa
h
R
i
v
e
r
Beech Flats Prong
Tuckasegee River
Culla
s
a
j
a
R
i
v
e
r
Little Tennessee River
Little Tennessee R.
T u c k a s e g e e River
Savan n ah Cree k
Tulula Creek
Forney C r e e k
Noland Cr e e k
C
a
rtoo g echaye Cr.
Nantahala R i v e r
Little
T
e
nnes
s
e
e River
So co Cree kDe
e
p Creek
O c o n aluftee R.
Caney F o r k
Hazel C re e k
Santeetlah Cr.
Ü024681
Miles
2010 Use Support
Supporting
No Data
Not Rated
Impaired
Municipalities
County Boundaries
Roads
Legend
d Stormwater
Permits
X Major Discharge
#0 Minor Discharge
Q Non-Discharge
Tuckasegee River
Subbasin 06010203
NC Division of Water Quality
Basinwide Planning Unit
Sept. 2011
Monitoring Sites
"à)Benthic Macroinvertebrate
[¡Fish¢¡Ambient¢¡RAMS ('07-'08)
^_Lake
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WateR QuaLity oveRvieW
The Tuckasegee River Subbasin, hydrologic
unit 06010203, was represented in previous
Basin Plans as Subbasin 04-04-02. This
subbasin covers 734 sq. miles and is 89%
forested; containing portions of Nantahala
National Forest and Great Smoky Mountains
National Park (Figure 1-1). There are
approximately 3,429 reservoir acres and
~998 classified stream miles, not including
the numerous unnamed tributaries. The
Tuckasegee River drains into Fontana Lake
just downstream of Bryson City.
This subbasin contains some of the most
pristine high quality waters in the state and
supports numerous trout streams (Figure
1-3). Water quality issues of concern in this
subbasin include impacts from developments
on steep slopes, agricultural runoff, stream
bank erosion, limited riparian cover and
individual onsite wastewater failures.
Waterbodies currently on the 2010 303(d)
list of Impaired waters include: a 1.3 mile
unnamed tributary to the Tuckasegee River,
Scott Creek, Sugarloaf Creek, Savannah
Creek and 170 acres of the Tuckasegee
River Arm of Fontana Lake. A map of
the subbasin showing Impaired streams,
monitoring and permit locations is shown in
Figure 1-2.
stReam FLoW
Stream flow is monitored at US Geological
Survey gaging stations. Flow, often abbreviated as
“Q”, is measured in terms of volume of water per
unit of time, usually cubic feet per second (cfs).
There are four gaging stations in this subbasin.
Figure 1-4 provides an example of average stream
flow over a 11 year period and gives an idea of
which years received heavier precipitation. For
more information about instream flow see DWR
website: http://www.ncwater.org/About_DWR/
Water_Projects_Section/Instream_Flow/welcome.
html.
The flow rate in a stream can impact the
measurement of physical and chemical
parameters. In particular, droughts can have major
affects on parameters such as dissolved oxygen,
turbidity, pH, and others by reducing stream flow.
Most recently this subbasin was in drought conditions in 2007 and 2008 (see page 17 AMS Report). Drought
effect on discharge in the Tuckasegee River was somewhat reduced by the almost daily releases of water
Figure 1-3: sTreaM CLassiFiCaTioNs
ORW
HQW / ORW Buffer
HQW
WSW I or II
HQW / WSW
Stream Classifications
Highlands
Franklin
S c o tt C reek
R
a
v
e
n For
k
Nantah
a
l
a
R
iver
Beech Flats Prong
Tuckasegee River
Cullasaja
R
i
v
e
r
Little Tennessee River
Tucka s eg e e River
Savan n ah Cree k
Forney C re e k
Noland Cr e e k
Ca
rtoo gechaye Cr.
Nantahala R iv er
Little
T
e
nnes
s
ee River
Soco Cree kDee
p Creek
Oc o n aluftee R.
Caney F o r k
H a z el C re e k
WS-IV
WS-IV,B;CA
WS-IV,B;ORW,CA
WS-IV;CA
WS-IV;Tr,CA
WS-IV;Tr,ORW
WS-IV;Tr,ORW,CA
WS-II,B;Tr,HQW,CA
WS-I;HQW
WS-I;Tr,HQW
WS-II,B;Tr,HQW
WS-II;HQW
WS-II;HQW,CA
WS-II;Tr,HQW
WS-II;Tr,HQW,CA
B
B;ORW
B;Tr
B;Tr,HQW
B;Tr,ORW
C
C;HQW
C;ORW
C;Tr
C;Tr,HQW
C;Tr,HQW:#
C;Tr,ORW
WS-III
WS-III,B;HQW
WS-III,B;Tr
WS-III,B;Tr,CA
WS-III,B;Tr,HQW
WS-III,B;Tr,ORW
WS-III:@
WS-III;CA
WS-III;HQW
WS-III;ORW
WS-III;Tr
WS-III;Tr,CA
WS-III;Tr,HQW
WS-III;Tr:@
For more information regarding stream classifications see:
http://portal.ncdenr.org/web/wq/ps/csu/
Figure 1-4: Stream flow at USGS 03513000 tUckaSeGee
river at BrySon city (yearly averaGe BaSed on daily meanS)
0
400
800
1200
1600
2000
200020012002 2003 2004 2005 2006 2007 2008 2009 2010
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from the Duke Energy hydroelectric facility at the lower end of the West Fork of the Tuckasegee River.
The Oconaluftee River, with no dam control, the drought effect was more pronounced. Annual average
streamflow for 2007 was the lowest in since data collection in ~1946. Low precipitation over the 2007-08
winter accentuated the drought with recovery not starting until the storms in November 2008.
bioLogicaL monitoRing
Biocriteria have been developed using the diversity, abundance, and pollution sensitivity of the organisms
that inhabit flowing waterbodies in NC. One of five bioclassifications are typically assigned to each water
body sampled: Excellent, Good, Good-Fair, Fair and Poor. Not Impaired and Not Rated designations are
reserved for samples that were not eligible to be assigned one of the five typical bioclassification categories.
Typically, a “Not Impaired” rating is equivalent to a Good-Fair or better bioclassification and a “Not Rated”
designation is equivalent to a Fair or worse bioclassification. The reasons for not being able to assign
one of these five typical bioclassifications may be a lack of appropriate bio-criteria or atypical sampling
conditions (e.g., drought). These bioclassifications are used to assess the various impacts of both point
source discharges and nonpoint source runoff. The resulting information is used to document both spatial
and temporal changes in water quality, and to complement water chemistry analyses, ambient toxicity data,
and habitat evaluations. In addition to assessing the effects of water pollution, biological information is also
used to define High Quality or Outstanding Resource Waters, support enforcement of stream standards,
and measure improvements associated with management actions. The results of biological investigations
have been an integral part in North
Carolina’s basinwide monitoring
program.
Biological samples were collected
during the spring and summer months
of 2004 and 2009-10 by the DWQ-
Environmental Sciences Section as
part of the five-year basinwide
sampling cycle. Fourteen benthic
macroinvertebrate sites and three fish
community sites were evaluated in
2009-10, representing seventeen
distinct localities. Each basinwide
biological station monitored during the
current cycle is shown in Figure 1-5
and color coded based on its current
rating. The majority of benthic
macroinvertebrate samples taken in
this watershed received an Excellent
rating. Several fish community sites
resulted in a Not Rated status, due to
the absence of criteria for rating high
gradient mountain trout waters, while
others rated Good. There were an
additional 8 samples taken at new
locations.
Benthos
Among the benthic macroinvertebrate sample sites, four sites improved,
two declined and eight retained the same bioclassification in 2009-2010
as observed in 2004. There were an additional four benthic samples taken
to support special studies. Figure 1-6 shows the distribution of these
samples.
Figure 1-5: bioLogiCaL siTes CurreNT raTiNgs
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Highlands
Sylva
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artoo g echaye Cr.
Nantahala Riv er
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Figure 1-6: beNThiC MaCroiNverTebraTe saMpLe sTaTus
22%
45%
11%
22%
Benthos
Improved
Unchanged
Declined
New Site
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Fish
Among the three fish community sites, two improved from 2004 while the
one remaining site maintained the same bioclassification in 2009 from that
observed in 2004. There were an additional four fish community samples
taken to support special studies. Figure 1-7 shows the distribution of
these samples.
For more information about biological data in this watershed, see the 2010
Little Tennessee River Basinwide Assessment Report. Detailed data sheets
for each sampling site can be found in Appendix 1-B.
Long teRm ambient monitoRing
The DWQ’s Ambient Monitoring System (AMS) is a network of stream stations strategically located for
the collection of physical and chemical water quality data. There is one AMS station (G8600000) in this
subbasin; data has been collected from this site since 1973. The following discussion of ambient monitoring
parameters includes concentration value graphs for AMS station G8600000 over a 11 year period (2000-
2010). Each major parameter is discussed, even if no current impairment exists. The graphs are not
intended to provide statistically significant trend information, but rather an idea of how changes in land use
or climate conditions can affect parameter readings over the long term. The difference between median and
mean results indicate the presence of outliers in the data set. Box and whisker plots of individual ambient
stations were completed by parameter for data between 2005 and 2009 by DWQ’s Environmental Sciences
Section (ESS) and can be found in the Little Tennessee River Basin Ambient Monitoring System Report.
pH
As seen in Figure 1-8, which represents the data window for the 2010 303(d) list, ambient site G8600000
had at least one sample that fell below the pH standard of 6su, but it did not exceed the standard in 10%
or more of the samples. Over 11 years (Figure 1-9), there were four incidences of pH dropping below the
minimal standard of 6 su at AMS G8600000.
At a Random Ambient Monitoring System site (G4210000) on an unnamed tributary to Tuckasegee River at
State Road 1172 near East Laport, samples taken recorded low pH levels resulting in Impairment.
Figure 1-7: Fish
CoMMuNiTy saMpLe sTaTus
29%
14%57%
Fish
Improved
Unchanged
Declined
New Site
Figure 1-8: PercentaGe of SamPleS
exceedinG the Ph <6 Standard
Between 2004-2008
Macon
0%< 7%7% - 10%>10%
Figure 1-9: SUmmarized Ph data at amS G8600000 Site Between 2000-2010
6.0
6.2
6.4
6.6
6.8
7.0
7.2
7.4
7.6
7.8
8.0
8.2
2000 2001 2002 2003 2004 2005 2006 2007 2008 2009 2010
pH
SU
Median
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Dissolved Oxygen
As seen in Figure 1-10, which represents the data window for the 2010 303(d) list, ambient station
G8600000 did not have any exceedances of DO standards. Over the past 11 years (Figure 1-11), no
samples were collected with dissolved oxygen levels below the 4mg/l instantaneous standard for Class C
waters.
Fecal Coliform Bacteria
Fecal coliform bacteria occurs in water as a result of the overflow of domestic sewage and from other
nonpoint sources of human and animal waste, including pets, wildlife and farm animals. The fecal coliform
bacteria standard for freshwater streams is not to exceed the geometric mean of 200 colonies/100 ml or 400
colonies/100 ml in 20% of the samples where five samples have been taken in a span of 30 days (5-in-30).
Only results from a 5-in-30 study are used to indicate whether a stream is Impaired or Supporting. Waters
with a use classification of B (primary recreational waters) are prioritized for 5-in-30 studies.
As seen in Figure 1-12, which represents the data window for the 2010 303(d) list, ambient station
G8600000 exceeded the 400 colonies/100ml in at least one sample. There were eight incidences of high
bacteria counts as indicated by several peaks in mean values over the eleven compared years, shown in
Figure 1-13 . There are three waterbodies Impaired because of elevated fecal coliform bacteria detected in
5-in-30 data collected in August 2005: Savannah Creek, Scott Creek and Tuckasegee River.
Figure 1-10: perCeNTage oF saMpLes
exCeeDiNg The Do <4 sTaNDarD
beTweeN 2004-2008
Macon
0%
< 7%
7% - 10%>10%
Figure 1-11: suMMarizeD Do DaTa aT aMs g8600000 siTe beTweeN 2000-2010.
6.0
7.0
8.0
9.0
10.0
11.0
12.0
2000 2001 2002 2003 2004 2005 2006 2007 2008 2009 2010
DO
m
g
/
L
Median Mean
Figure 1-12: PercentaGe of
SamPleS exceedinG the fecal
coliform Bacteria >400
Standard Between 2004-2008
Macon
0%
< 7%
7% - 10%>10%
Figure 1-13: SUmmarized fecal coliform Bacteria data at amS
G8600000 Site Between 2000-2010.
0.0
50.0
100.0
150.0
200.0
250.0
300.0
350.0
400.0
2000 2001 2002 2003 2004 2005 2006 2007 2008 2009 2010
Fe
c
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C
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o
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(c
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Turbidity
As seen in Figure 1-14, which represents the data window for the 2010 303(d) list, ambient site G8600000
did not have any samples that exceeded 50NTUs. Over the past 11 years (Figure 1-15), only one sample at
exceeded the standard of >50 NTUs for Class C waters.
PRotection anD RestoRation oPPoRtunities
The following section provides more detail about specific streams where special studies have occurred
or stressor sources information is available. Within this document, biological sample site IDs ending in an
“F” denote fish community and a “B” denote macroinvertebrate community. Specific stream information
regarding basinwide biological samples sites are available in Appendix 1B. Use support information on all
monitored streams can be found in Appendix 1A. Detailed maps of each of the watersheds are found in
Appendix 1C or by clicking on the following small maps.
To assist in identifying potential water quality issues citizens, watershed groups and resource agencies can
gather and report information through our Impaired and Impacted Stream/ Watershed survey found here:
http://portal.ncdenr.org/web/wq/ps/bpu/about/impactedstreamssurvey.
uPPeR tuckasegee RiveR WateRsHeD (Huc 0601020301)
This watershed encompasses 152,466 acres and has an estimated 2010 population
of 15,325 people. A majority of the watershed is within a WS-III area.
West Fork Tuckasegee River/ Thorpe Lake [2-79-23-(1)] (WS-III,B;HQW)
also known as Glenville Lake, is a man-made
impoundment on the Tuckasegee River located in
Jackson County. The lake is used for recreational
fishing, swimming, and boating. Owned by Duke
Energy, the reservoir also has been used for
hydroelectric power generation since its construction in 1941. Thorpe
Lake was monitored by DWQ in 2009, which determined the Lake is still
oligotrophic as it has been since it was first monitored in 1988. Trillium
Figure 1-14: PercentaGe of SamPleS
exceedinG the >50 tUrBidity Standard
Between 2004-2008
Macon
0%< 7%
7% - 10%>10%
Figure 1-15: SUmmarized tUrBidity data at amS G8600000 Site
Between 2000-2010.
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
9.0
10.0
11.0
12.0
2000 2001 2002 2003 2004 2005 2006 2007 2008 2009 2010
Tr
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N
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Links & Village WWTP discharges into Hurricane Creek which a tributary to Thorpe Lake. The facility has
had several permits violations over the past five years, including exceedances for BOD, TSS, ammonia and
low DO.
Wolf Creek (Wolf Creek Lake) [2-79-9-(1)] (WS-III,B;Tr,HQW) Wolf Creek Reservoir is a small hydroelectric
reservoir built by Nantahala Power and Light Company in 1955 on the Tuckasegee River and is currently
owned by Duke Energy. Wolf Creek Reservoir has a forested watershed. The shoreline of the lake has a
relatively low density of private homes, however evidence of land clearing and new home construction was
observed in 2009. Monitoring by DWQ field staff of Wolf Creek Lake was conducted monthly from May
through September, 2009. Data collected indicated that the lake’s trophic state to be oligotrophic. This
trophic state has not changed since monitoring by DWQ began in 1988.
Tuckasegee River [AU# 2-79-(0.5)] (WS-III,B;Tr,ORW) was sampled at site GB38 in 2009 resulting in an
Good benthos bioclassification.
Tuckasegee River/ Bear Creek Lake [2-79-(5.5)b & 2-79-(5.5)c] (WS-III,B;Tr)
is a hydroelectric impoundment of the Tuckasegee River. Most of the 194 mi2
upland drainage area is forested with steep slopes and clean, fast-moving
streams. Bear Creek Lake was built in 1953 and is currently owned by Duke
Energy. DWQ field staff monitored Bear Creek Lake five times from May
through September in 2009. This reservoir has remained oligotrophic since
it was first monitored by DWQ in 1994. In past evaluations of Bear Creek
Reservoir, it was observed that the shoreline was predominantly forested with
a relatively undisturbed drainage area that helped to maintain the reservoir’s
low nutrient concentration and very clear water. It was noted in 2009 that residential development has
significantly increased along the shoreline and in the watershed of this reservoir.
Tuckasegee River/ Cedar Cliff Lake [2-79-(5.5)c] (WS-III,B;Tr) is a picturesque mountain lake on the
Tuckasegee River. The lake is owned by Duke Energy and was built in 1952. Water quality in the lake
supports swimming, boating, and trout fishing. The name of the lake was probably derived from a sheer rock
cliff, which faces it from the north. This lake was sampled in 2009 by DWQ, which determined the Lake is
still oligorophic as it has been since it was first monitored in 1988.
Unnamed tributary to Tuckasegee River [2-79-(24)ut4] was sampled for macroinvertebrate communities
in 2007 resulting in a Not Impaired status. A Random Ambient Monitoring System site (G4210000) also
collected data along this tributary between Jan. 2007 - Dec. 2008. Data collected included normal field
parameters along with metals, volatile organics, semi-volatiles, and pesticides. Over 18% of the samples
had low pH, but no other water quality problems were detected. This creek is now Impaired for Aquatic Life
because of the low pH levels.
Caney Fork [AU# 2-79-28-(2.5)] (WS-III;Tr) drains a small portion of east-central Jackson County, a mostly
forested landscape, and ultimately feeds into the Tuckasegee River. Caney Fork, for most of it’s length, is
paralleled by roadway and is lined by agricultural fields and residences. The stream is lacking significant
riparian vegetation and is often denuded on both sides streambanks. However, most of the watershed is
forested thereby protecting the Excellent water quality that has persisted in Caney Fork over the last two
decades. The stream was sampled at sites GB27 and GF4 resulting in an Excellent benthos and Good fish
community bioclassifications.
Moses Creek [2-79-28-8] (WS-III;Tr) is a tributary of Caney Fork. This stream has a catchment that is largely
forested with only the lower segment paralleling a rural residential road. It was noted that riparian loss was
occurring due to residential lawns, some upstream agriculture, and the nearby road. The Creek was sampled
at site GB26 in 2010 resulting in an Excellent benthos rating.
Cullowhee Creek [AU# 2-79-31a & b] (C;Tr ) flows north through Jackson County in the southwestern portion
of North Carolina. The majority of the headwaters are forested and of good water quality. The lower portion
of the watershed includes Western Carolina University, light commercial, and residential development.
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The stream through this section was historically moved and channelized resulting in poor habitat and flood
protection. In 2009, DWQ sampled Cullowhee Creek at two locations upstream of the university. The benthic
community at site GB29 rated Excellent, and the fish community at GF13 received a Good bioclassification.
The biologists noted high levels of sand, silt and macrophytes. Although Cullowhee Creek rated as Excellent
in 2009, habitat degradation is an issue and may negatively affect the fauna in the future.
oconaLuFtee RiveR WateRsHeD (Huc 0601020302)
This watershed encompasses 120,226 acres and has an estimated 2010 population
of 8,833 people.
Bradley Fork {AU# 2-79-55-12-(11)] (B;Tr,HQW) a tributary to the Oconaluftee
River, is located within Great Smoky Mountain National Park and as such has a
completely undeveloped and forested watershed. This stream has high recreational
usage among the public as it lies next to a campground just inside the park border
The creek was sampled in 2009 at site GB1 resulting in an Excellent benthos
bioclassification.
Oconaluftee River [AU# 2-79-55-(16.5)] (C;Tr) is a large tributary to the Tuckasegee River draining the
eastern portion of Great Smoky Mountain National Park. The lower segment of this river is tracked on both
sides by roads and receives large amounts of urban runoff from Cherokee. High development pressures
have introduced sediments into the river and removed large amounts of riparian vegetation. The River was
sampled in 2009, at site GB11, resulting in an Excellent benthos bioclassification, however the Excellent
rating is likely supported from the unimpacted tributaries as conditions in the Oconaluftee River itself are
deteriorating.
miDDLe tuckasegee RiveR WateRsHeD (Huc 0601020303)
This watershed encompasses 104,486 acres and has an estimated 2010 population
of 19,373 people.
Savannah Creek [AU# 2-79-36] (C;Tr ) watershed drains the west-central portion of
Jackson County. Savannah Creek itself flows alongside US 441 and NC 116 for
much of its length before joining the Tuckasegee River near Webster. Traditionally,
land use in the watershed was agricultural with light residential and commercial
activity along the transportation corridors. Residential development is increasing
substantially and elevating sediment and erosion concerns. DWQ does not have an
ambient monitoring station but DWQ did sample fecal coliform bacteria concentrations in Savannah Creek
as part of a Class B (Recreation) use-attainability study for the Tuckasegee River initiated in 2003. The
samples exceeded state standards and indicate Savannah Creek, from its source to the Tuckasegee River
(13.4 miles), is Impaired in the recreation category. The sources of fecal coliform contamination are
unknown, but may include failing septic systems and/or agricultural runoff. DWQ also sampled the fish and
benthic communities at sites GF23 and GB23, both resulting in Excellent ratings. However, these data do
not reflect the habitat threats posed by development in the watershed. Many stream reaches have been
channelized and riparian vegetation removed.
The Watershed Association for the Tuckasegee
River (WATR) is currently writing a watershed plan
and coordinates sampling in the Savannah Creek
Watershed. Data collected at Savannah Creek and
its largest tributary, Greens Creek, from July 2003
through September 2010 show turbidity levels that
exceed the 10 NTU standard for trout habitat waters.
savannaH ck.gReens ck.
n 89 87
exceeDing 10 ntus ~37%~33%
mean 19.4 9.7
meDian 7.7 7.5
maximum 450 80
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Measurements exceeded turbidity standards 37% of the time for Savannah Creek and 33% for Greens
Creek [AU# 2-79-36-11]. These results were obtained despite the regional drought conditions. Monthly
sampling also detected high flow and high turbidity conditions during the summers of 2007 and 2008.
WATR notes that DWQ’s sample site at NC116 is not representative
of stream conditions. The monitoring site at bridge on NC116 has
a relatively large gradient as compared to stream reaches up and
downstream. The station occupies a small water gap in a local ridge and
it has a rocky substrate. These factors combine to yield a short zone
that does not accumulate deposited sediments and is favorable habitat
for macroinvertebrates WATR recommends that if it is necessary to
acknowledge this biologically productive stream segment, then Savannah
Creek should be divided into three assessment reaches. Moving
upstream from the confluence, the first reach is a section of stream that
is characterized by low gradient. It passes through a wide floodplain with
agriculture, and stream banks are unstable and eroding. The second
assessment reach starts with the high gradient segment at Bridge along NC116. In the upstream
direction it forms a large curve in an isolated patch of flood plain, again dedicated to agriculture. This
reach extends into a larger water gap paralleled by Rt 116. The high gradient section in the water gap, a
place frequented by anglers, marks the upper end of this section. The third assessment reach starts at
the mid point in the water gap and extends upstream for the remaining length of Savannah Creek.
Since the temporary moratorium on construction in 2008 and the downturn in home building in 2009,
the relative effect of construction on erosion and turbidity has decreased significantly. Enforcement, and
especially clarity and enforcement of temporary and final vegetative cover, remains critically important
to improving water quality in the Savannah Creek watershed. Developing agriculture buffers and public
education on maintaining fallow land, road ways and road ditches are recommended. Fecal coliform
contamination sources in the Savannah Creek watershed should be identified and corrected. Additionally,
sediment and erosion control problems should be addressed to prevent further habitat degradation.
Water Quality Initiatives
WATR is working diligently to inform the public on the critical role of stream side buffers in maintaining a
healthy aquatic ecology and good water quality. Partnering with the Town of Dillsboro WATR volunteers and
staff have build the Stream Buffer Demonstration Trails at Monteith Farmstead Park. These short nature
trails with educational signs are specifically aimed at informing the landowners, and stream-side landowners
in particular, about the necessity of riparian buffers to healthy mountain streams. This work has been
supported by Resourceful Communities Program. WATR also has conducted youth environmental education
events funded by the Cherokee Preservation Foundation, the USDA Natural Resources Conservation
Service, and by WATR members and contributors.
Scott Creek [AU# 2-79-39] (C;Tr) is a large,
swift tributary to the Tuckasegee River. Draining
northeastern Jackson County, US 19/23 and Old
US 19/23 parallel the creek is for most of its length.
The stream passes through many residential
areas before entering the urban environment in
Sylva and Dillsboro. DWQ sampled fecal coliform
bacteria concentrations in Scotts Creek as part of
a Class B Recreation use-attainability study for the
Tuckasegee River initiated in 2003. The samples
exceeded state standards and indicate Scotts
Creek, from its source to the Tuckasegee River
(15.3 miles), is Impaired in the recreation category. Rafting on Scott Creek
The sources of fecal coliform contamination are unknown, but may include failing septic systems, leaking
sewer systems and/or nonpoint source runoff. In 2009, DWQ evaluated the benthic macroinvertebrate
community at site GB167 resulting in an Excellent bioclassification. This is an noted improvement compared
to the 2004 conditions, however the Creek still has turbidity and habitat issues. The stream channel is highly
modified and the bank is armored by riprap.
The Morningstar of Jackson WWTP facility discharges into Blanton Branch (AU# 2-79-39-10) which is a
tributary to Scott Creek. In 2010 the facility exceeded fecal coliform bacteria levels.
A small pond dam failure in the Balsam Mountain Preserve development occurred on June 7, 2007.
The resultant sediment and debris slide entered Sugarloaf Creek [AU# 2-79-39-5-1] (C) and finally the
lower segments of Scott Creek. A special benthos study was completed in 2007 to assess the impacts
from the dam failure. A total of three streams were sampled in this study. Two of the streams sampled
(Sugarloaf Creek and Scott Creek) were directly affected by the sediment. The third stream, Licklog
Branch [2-79-39-3-6] (C), was sampled as a comparative reference site to Sugarloaf Creek and was
similar in both landuse and drainage area. Results of the study indicate that the dam failure did affect the
macroinvertebrate community in Sugarloaf Creek as it had a “Fair” bioclassification while the reference
site was “Good”. The downstream reaches of Scott Creek received an “Excellent” bioclassification.
Tuckasegee River [2-79-(35.5)a & 2-79-(35.5)b & 2-79-(38)] (C;Tr) receives effluent from the municipalities
of Sylva, Webster, and Dillsboro and drains almost the entirety of Jackson County. The River is Impaired for
recreational uses due to exceedances of the fecal coliform bacteria levels. The Jackson County WWTP has
had numerous permit violations within the five years, including exceedances in fecal coliform bacteria, BOD,
TSS levels and low pH.
Downstream [AU# 2-79-(40.5)] the in the Tuckasegee River a biological sample was taken in 2009 at site
GB19 resulting in an Good benthos bioclassification. The most significant event for aquatic biology in the
Tuckasegee River watershed was the removal of the low-head dam at Dillsboro in early winter of 2009. Prior
to dam removal, Duke Energy pumped out and removed much of the impounded sediment. Dam removal
allows fish species to migrate upstream, with the potential for host species for the endangered Appalachian
Elktoe Mussel to also migrate upstream. As part of the dam removal, the river bank along the former
impoundment has been restored with stone armoring at the toe of the slope affected by water level changes
caused by daily discharge related to hydroelectric generation.
Camp Creek [AU# 2-79-49] (C) watershed, including the Beck Branch [AU# 2-79-49-1] (C) watershed,
encompasses approximately 4.5 square miles in northwestern Jackson County. The creek is a tributary to
the Tuckasegee River. Visible landuses in the watershed include forest, rural residential, infrastructure
(secondary roads and US 441), commercial, active pastures, horse pastures, and fallow fields. There is one
NPDES permitted discharger to Camp Creek (NC0074250) with no recent permit violations. DWQ received a
request to reclassify Camp Creek to trout waters in 2004. In 2005, the fish community was sampled at
several sites in the Camp Creek watershed to determine if determine if there were wild, reproducing
populations of trout in Camp Creek and Beck Branch. The survey did indicate significant habitat problems in
the watershed. The primary habitat problems were unstable, eroding stream banks, and narrow or non-
existent riparian vegetation. In this Camp Creek reclassification/use attainability study, it was determined
after sampling 4 locations that only the upper 2.3 square mile watershed of the creek met the trout waters
regulation criteria. Suitable instream habitats were present at the lower two sites on Camp Creek for trout,
but the lack of wide forested riparian zones and nonpoint source runoff may prevent their occupation of
those reaches of the creek on a year-round basis. Stream restoration activities would benefit the likelihood
of trout recolonizing, inhabiting on a year-round basis, and reproducing in the middle and lower reaches of
the creek. (memorandum 20050605).
nPDes PeRmits WitHin tHe miDDLe tuckasegee RiveR WateRsHeD
Permit #Permit TypeOutfall locationFacility Name
NCG210134StormwaterScott CrT&S Hardwoods Inc
NCG100168StormwaterScott CrDr Automotive
NC0032808WWTPBlanton BrMorningstar of Jackson
NCG050383StormwaterScott CrStonewall Packaging, LLC
NCG080191StormwaterYellow Bird BrUnited Parcel Service Inc
WQ0005207Non-dischargeWastewater
RecyclingJackson Paper Manufacturing Company
NCG140158StormwaterScott CrSouthern Concrete Materials Inc
NC0020214WWTPScott CrSylva WWTP
NCG551046WastewaterSavannah Crsingle family residence
NCG080730
NCG080731StormwaterSouth Fork Blair
CrRolling Frito-Lay
WQ0005763Non-dischargeBiosolidsTuckaseigee Water & Sewer Authority
NC0039578WWTPTuckasegee RJackson County WWTP
NCG110111StormwaterTuckasegee RTuckaseigee Water & Sewer Authority
NCG160031StormwaterTuckasegee RDillsboro Asphalt Plant
NCG020247StormwaterTuckasegee RDillsboro Quarry
NCS000295StormwaterScott CrJackson Paper Manufacturing Company
NCG550375WastewaterW Fork Dicks Crsingle family residence
NC0074250WWTPCamp CreekGateway Chevron
NC0000264WWTPTuckasegee RJackson Co Industrial Park
NC0084441WWTPConnelly CrSmoky Mountain Country Club
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The sources of fecal coliform contamination are unknown, but may include failing septic systems, leaking
sewer systems and/or nonpoint source runoff. In 2009, DWQ evaluated the benthic macroinvertebrate
community at site GB167 resulting in an Excellent bioclassification. This is an noted improvement compared
to the 2004 conditions, however the Creek still has turbidity and habitat issues. The stream channel is highly
modified and the bank is armored by riprap.
The Morningstar of Jackson WWTP facility discharges into Blanton Branch (AU# 2-79-39-10) which is a
tributary to Scott Creek. In 2010 the facility exceeded fecal coliform bacteria levels.
A small pond dam failure in the Balsam Mountain Preserve development occurred on June 7, 2007.
The resultant sediment and debris slide entered Sugarloaf Creek [AU# 2-79-39-5-1] (C) and finally the
lower segments of Scott Creek. A special benthos study was completed in 2007 to assess the impacts
from the dam failure. A total of three streams were sampled in this study. Two of the streams sampled
(Sugarloaf Creek and Scott Creek) were directly affected by the sediment. The third stream, Licklog
Branch [2-79-39-3-6] (C), was sampled as a comparative reference site to Sugarloaf Creek and was
similar in both landuse and drainage area. Results of the study indicate that the dam failure did affect the
macroinvertebrate community in Sugarloaf Creek as it had a “Fair” bioclassification while the reference
site was “Good”. The downstream reaches of Scott Creek received an “Excellent” bioclassification.
Tuckasegee River [2-79-(35.5)a & 2-79-(35.5)b & 2-79-(38)] (C;Tr) receives effluent from the municipalities
of Sylva, Webster, and Dillsboro and drains almost the entirety of Jackson County. The River is Impaired for
recreational uses due to exceedances of the fecal coliform bacteria levels. The Jackson County WWTP has
had numerous permit violations within the five years, including exceedances in fecal coliform bacteria, BOD,
TSS levels and low pH.
Downstream [AU# 2-79-(40.5)] the in the Tuckasegee River a biological sample was taken in 2009 at site
GB19 resulting in an Good benthos bioclassification. The most significant event for aquatic biology in the
Tuckasegee River watershed was the removal of the low-head dam at Dillsboro in early winter of 2009. Prior
to dam removal, Duke Energy pumped out and removed much of the impounded sediment. Dam removal
allows fish species to migrate upstream, with the potential for host species for the endangered Appalachian
Elktoe Mussel to also migrate upstream. As part of the dam removal, the river bank along the former
impoundment has been restored with stone armoring at the toe of the slope affected by water level changes
caused by daily discharge related to hydroelectric generation.
Camp Creek [AU# 2-79-49] (C) watershed, including the Beck Branch [AU# 2-79-49-1] (C) watershed,
encompasses approximately 4.5 square miles in northwestern Jackson County. The creek is a tributary to
the Tuckasegee River. Visible landuses in the watershed include forest, rural residential, infrastructure
(secondary roads and US 441), commercial, active pastures, horse pastures, and fallow fields. There is one
NPDES permitted discharger to Camp Creek (NC0074250) with no recent permit violations. DWQ received a
request to reclassify Camp Creek to trout waters in 2004. In 2005, the fish community was sampled at
several sites in the Camp Creek watershed to determine if determine if there were wild, reproducing
populations of trout in Camp Creek and Beck Branch. The survey did indicate significant habitat problems in
the watershed. The primary habitat problems were unstable, eroding stream banks, and narrow or non-
existent riparian vegetation. In this Camp Creek reclassification/use attainability study, it was determined
after sampling 4 locations that only the upper 2.3 square mile watershed of the creek met the trout waters
regulation criteria. Suitable instream habitats were present at the lower two sites on Camp Creek for trout,
but the lack of wide forested riparian zones and nonpoint source runoff may prevent their occupation of
those reaches of the creek on a year-round basis. Stream restoration activities would benefit the likelihood
of trout recolonizing, inhabiting on a year-round basis, and reproducing in the middle and lower reaches of
the creek. (memorandum 20050605).
nPDes PeRmits WitHin tHe miDDLe tuckasegee RiveR WateRsHeD
Permit #Permit TypeOutfall locationFacility Name
NCG210134StormwaterScott CrT&S Hardwoods Inc
NCG100168StormwaterScott CrDr Automotive
NC0032808WWTPBlanton BrMorningstar of Jackson
NCG050383StormwaterScott CrStonewall Packaging, LLC
NCG080191StormwaterYellow Bird BrUnited Parcel Service Inc
WQ0005207Non-dischargeWastewater
RecyclingJackson Paper Manufacturing Company
NCG140158StormwaterScott CrSouthern Concrete Materials Inc
NC0020214WWTPScott CrSylva WWTP
NCG551046WastewaterSavannah Crsingle family residence
NCG080730
NCG080731StormwaterSouth Fork Blair
CrRolling Frito-Lay
WQ0005763Non-dischargeBiosolidsTuckaseigee Water & Sewer Authority
NC0039578WWTPTuckasegee RJackson County WWTP
NCG110111StormwaterTuckasegee RTuckaseigee Water & Sewer Authority
NCG160031StormwaterTuckasegee RDillsboro Asphalt Plant
NCG020247StormwaterTuckasegee RDillsboro Quarry
NCS000295StormwaterScott CrJackson Paper Manufacturing Company
NCG550375WastewaterW Fork Dicks Crsingle family residence
NC0074250WWTPCamp CreekGateway Chevron
NC0000264WWTPTuckasegee RJackson Co Industrial Park
NC0084441WWTPConnelly CrSmoky Mountain Country Club
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Conley Creek (Connelly Creek) [2-79-52] (C;Tr) is a small tributary to the Tuckasegee River and drains a
small portion of southeastern Swain County. Only the lower portion of the watershed is developed, consisting
mostly of residences and a golf course, while majority of the upper watershed is forest. The stream follows a
road for much of its length which has reduced or removed the riparian on one side for much of the segment.
However, overall habitat was good and the stream banks were stable with little erosion. The Creek was
sampled in 2009 resulting in an Excellent benthos bioclassification.
LoWeR tuckasegee RiveR WateRsHeD (Huc 0601020304)
This watershed encompasses 92,429 acres and has an estimated 2010 population of
5,630 people. A majority of the watershed (the northern portion) falls within the Great
Smoky Mtn National Park.
Deep Creek [2-79-63-(16) & 2-79-63-(21)] (B;Tr) flows through a primarily forested
area and has high recreational use draining into the Tuckasegee River. The lower
1.8 miles of the creek are not within the Great Smoky Mtns National Park and the
land use turns to agriculture. Sedimentation was noted in this reach of the Creek
but not enough to prevent the sample site GB7 from receiving an Excellent benthos
bioclassification. The Creek has maintained an Excellent rating for the last 20 years.
However, Deep Creek experienced effluent overflow from a sewer spill in 2010 that was captured on video.
The video can be viewed through this youtube link: http://www.youtube.com/user/RogerWATR
Noland Creek [2-90] (C;Tr) lies within the south central portion Great Smoky Mountain National Park and
drains into Fontana Lake. It is an undeveloped and forested watershed. The habitat of Noland Creek is
exceptional and consists of a series of cascades, riffles, and pools; site GB6 rated Excellent in 2009.
Forney Creek [2-97] (C;Tr,ORW) lies within and drains the south-central portion of Great Smoky Mtns
into Fontana Lake. It is an entirely undeveloped and forested watershed. The habitat of this stream is
as expected for a stream in a natural setting and consists of a series of riffles, cascades, and pools with
excellent riparian zones. The Creek rated Excellent in 2009 at site GB4.
Tuckasegee River [2-(78)a] (C) downstream of Bryson City from Lemmons Creek to Peachtree Creek is
Impaired for Recreational uses due to exceedances of fecal coliform bacteria levels. Just upstream is AMS
station G8600000 which also detected high levels of fecal coliform bacteria and had several incidences of
low pH. Bryson City’s WWTP discharges into the Tuckasegee River and over the last five years has had
several incidences of permit violations, including fecal coliform bacteria and TSS.
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notabLe WateRs
Table 1-1 lists waterbodies identified as needing additional protection and potential restoration actions. The
fourth and fifth columns of this table list potential stressors and sources that may be impacting a stream
based on in-field observations, monitoring data, historical evidence, permit or other violations, and other staff
and public input. In many cases, additional study is needed to determine exact source(s) of the impact. The
last column includes a list of recommended actions.
TabLe 1-1: NoTabLe waTers
Stream Name AU#Class.Stressor Source Status Actions
Needed
Cullowhee Creek 2-79-31a 2-79-31b C;Tr sediment, nutrients development S S&E, P
Oconoaluftee R 2-79-55-(16.5)C;Tr sediment development S S&E, P
Savannah Creek 2-79-36 C;Tr
fecal coliform
bacteria,
sediment
development, agriculture, failing
septic systems
I S&E,
BMPs
Scott Creek 2-79-39 C;Tr
fecal coliform
bacteria,
sediment
non-point source runoff, failing
septic systems, impoundments
I R,
BMPs
Tuckasegee R
2-79-(35.5)a
2-79-(35.5)b
2-79-(38)
[2-(78)a
C; Tr
C; Tr
C
C
fecal coliform
bacteria WWTP, non-point source runoff I BMPs
AU # = Assessment Unit # or stream segment/reach
Class. = Classification (e.g., C, S, B, WS-I, WS-II, WS-III, WS-IV, WS-V, Tr, HQW, ORW, SW, UWL)
Stressor = chemical parameters or physical conditions that at certain levels prevent waterbodies from meeting the standards for their designated use.(e.g., low/high DO, nutrients, toxicity, habitat degradation, etc. )
Status = I=Impaired, IM= Impacted, S=Supporting, IP= Improving,
Actions Needed = R= restoration, P= protection, SC= stormwater controls, SS= stressor study, E= education, LO=
local ordinance, BMPs, SSP= species protection plan, F= forestry BMPs, Ag= Agriculture BMPs, NMC= nutrient mgnt
controls, S&E= sediment and erosion controls
TabLe 1-2: NpDes perMiTs wiThiN The TuCkasegee river subbasiN
nPDes PeRmits WitHin tHe tuckasegee RiveR subbasin
PeRmit #PeRmit tyPe outFaLL Location FaciLity name
nPDes PeRmits WitHin tHe uPPeR tuckasegee RiveR WateRsHeD
NC0075736 WWTP Grassy Swamp Cr Whiteside Estates Inc
WQ0017530 Non-discharge irrigation Highlands Cove
WQ0028693 Non-discharge reuse Mountaintop Golf & Lake Club
NC0066958 WWTP Hurricane Cr Blue Ridge School
NC0059200 WWTP Hurricane Cr Trillium Links & Village LLC
NC0038687 WWTP Trout Cr Singing Waters Camping Resort
WQ0031427 Non-discharge irrigation Legasus of North Carolina LLC
NCG500127 Wastewater W Fork Tuckasegee R Thorpe Hydroelectric Station
NCG500126 Wastewater W Fork Tuckasegee R Tuckasegee Hydroelectric Station
NCG500125 Wastewater W Fork Tuckasegee R Cedar Cliff Hydroelectric Station
NCG500124 Wastewater W Fork Tuckasegee R Bear Creek Hydroelectric Plant
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nPDes PeRmits WitHin tHe tuckasegee RiveR subbasin
PeRmit #PeRmit tyPe outFaLL Location FaciLity name
NCG500123 Wastewater Tennessee Cr Tennessee Cr Hydroelectric Station
WQ0029233 Non-discharge reuse Bear Lake Reserve
NCG550374 Wastewater Tilley Cr Cullowhee Valley Baptist Church
NCG510066 groundwater remediation Tuckasegee R Lewis Oil Company
NC0074624 WTP Tuckasegee R Western Carolina University
NCG150027 Stormwater Ditch to Tuck. R Jackson County Airport
nPDes PeRmits WitHin tHe oconaLuFtee WateRsHeD
NCG500129 Wastewater Oconaluftee R Bryson Hydroelectric Station
nPDes PeRmits WitHin tHe miDDLe tuckasegee RiveR WateRsHeD
NCG210134 Stormwater Scott Cr T&S Hardwoods Inc
NCG100168 Stormwater Scott Cr Dr Automotive
NCG050383 Stormwater Scott Cr Stonewall Packaging, LLC
NCG140158 Stormwater Scott Cr Southern Concrete Materials Inc
NCS000295 Stormwater Scott Cr Jackson Paper Manufacturing Co.
NC0020214 WWTP Scott Cr Sylva WWTP
NC0032808 WWTP Blanton Br Morningstar of Jackson
NCG080191 Stormwater Yellow Bird Br United Parcel Service Inc
WQ0005207 Non-discharge Wastewater Recycling Jackson Paper Manufacturing Co.
NCG551046 Wastewater Savannah Cr single family residence
NCG080730
NCG080731 Stormwater South Fork Blair Cr Rolling Frito-Lay
WQ0005763 Non-discharge Biosolids Tuckasegee Water & Sewer Authority
NC0000264 WWTP Tuckasegee R Jackson Co Industrial Park
NC0039578 WWTP Tuckasegee R Jackson County WWTP
NCG110111 Stormwater Tuckasegee R Tuckasegee Water & Sewer Authority
NCG160031 Stormwater Tuckasegee R Dillsboro Asphalt Plant
NCG020247 Stormwater Tuckasegee R Dillsboro Quarry
NCG550375 Wastewater W Fork Dicks Cr single family residence
NC0074250 WWTP Camp Creek Gateway Chevron
NC0084441 WWTP Connelly Cr Smoky Mountain Country Club
nPDes PeRmits WitHin LoWeR tuckasegee RiveR WateRsHeD
NCG530095 Wastewater Cooper Cr Cooper Creek Trout Farm
NC0061620 WWTP Tuckasegee R Hide Away Campground
NC0026557 WWTP Tuckasegee R Town of Bryson City
NCG210098
NCG210095 Stormwater Tuckasegee R Powell Industries
WQ0005557 Non-discharge Wastewater Recycling Mini Apolis Grand Prix Corp
NCG050249 Stormwater Cochran Br Consolidated Metco Inc
NCG140395 Stormwater Cochran Br Southern Concrete Materials Inc
NCG210392 Stormwater ditch to Cochran Br Zickgraf Hardwood Flooring LLC
NCG160199 Stormwater ditch to Cochran Br Hmc Paving & Construction Co Inc
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ReFeRences & useFuL Websites
NC Division of Water Quality
Biological Assessment- http://portal.ncdenr.org/c/document_library/get_file?uuid=de0dbb2d-3417-
44c4-9736-1710d2e18d43&groupId=38364
Ambient Report- http://portal.ncdenr.org/c/document_library/get_file?uuid=ac3b7afe-e2f1-4d1e-93df-
c2ba9d897888&groupId=38364
Lakes & Reservoir Assessment- http://portal.ncdenr.org/c/document_library/get_file?uuid=0b586b2a-
6851-4783-a4e1-a7f58b2549f4&groupId=38364
303(d) List- http://portal.ncdenr.org/web/wq/ps/mtu/assessment
Impaired & Impacted Survey- http://portal.ncdenr.org/web/wq/ps/bpu/about/impactedstreamssurvey
NC Division of Water Resources
Flow- http://www.ncwater.org/Permits_and_Registration/Instream_Flow/
Watershed Association for the Tuckasegee River (WATR)
http://watrnc.wordpress.com/