|
Map of Watershed Sample Sites [Popup PDF]
List of Watershed Sample Sites [Popup]
Named
Streams
Pocono Creek
- Little Pocono Creek
- Big Meadow Run
- Flagler Run
- Wigwam Run
- Rocky Run
- Reeders Run
- Coolmoor Creek
- Cranberry Creek
- Bulgers Run
- Scot Run
- Wolf Swamp Run
- Sand Spring Run
- Dry Sawmill Run
 Municipalities
- Pocono Township
- Jackson Township
- Stroud Township
- Stroudsburg Borough
- Tobyhanna Township
- Tunkhannock Township
Named
Lakes, Ponds, and Impoundments
- Wolf Swamp Run Dam (on Wolf Swamp Run)
- Pine Tree Lake (on Dry Sawmill Run)
- Emerald Lakes/Youngs Pond (on Dry Sawmill Run)
- Crescent Lake (on Dry Sawmill Run)
- Mountaintop Lake (on Dry Sawmill Run)
- Wilson Dam (on Dry Sawmill Run)
- Deer Pond (on Dry Sawmill Run)
- Little Deer Pond (on Dry Sawmill Run)
- Deep Lake (on Sand Spring Run)
- Lindemere Dam (on Pocono Creek)
- Barneys Pond (on Pocono Creek)
- Camelback Reservoir (on Pocono Creek)
- Shaeff & Peters Dam (on Pocono Creek)
- Brookdale Lake (on Scot Run)
- Leisure Lake (on Scot Run)
- Massad Camp Dam (on Scot Run)
- Noah's Ark Dam (on Scot Run)
- Hemlock Lake (on Cranberry Creek)
- Hunter Lake (on Rocky Run)
- Lenape Lake (on Rocky Run)
- Wigwam Lake (on Wigwam Run)
- Flagler Dam (on Flagler Run)
- Lower Dam (on Flagler Run)
- Laurel Lake (on Laurel Run)
- Twin Hills Dam (on Little Pocono Creek)
Did
You Know?
The Pocono Creek drains the Pocono Plateau in its headwaters in Tobyhanna
and Tunkhannock Townships and flows for 16 miles in a southeastern direction
through Pocono, Jackson, Hamilton and Stroud Townships where it converges
with the McMichael Creek in Stroudsburg. The Pocono watershed drains a
surface area of approximately 48 square miles and contains 14 sub-basins
within its boundaries. The Pocono Creek is paralleled by Interstate-80
and the county's primary commercial artery, Route 611, which was built
in the floodplain. Intense commercial development occurs along and near
the stream in the middle and southerly sections of the watershed.
The Pocono Plateau escarpment forms the watershed's most prominent topographic
feature, Big Pocono Mountain, which forms the western watershed boundary.
The watershed includes the Tannersville Cranberry (peat) Bog, which is
believed to have formed during a glacial retreat. The Cranberry Bog is
the southernmost alpine boreal bog in the United States and is found in
the east-central portion of the watershed. A large portion of the bog
is protected through ownership and management by the Nature Conservancy.
The Bog forms the eastern edge of the watershed.
The major tributaries running south into the Pocono Creek are Dry Sawmill
Run, Sand Spring Run, Wolf Swamp Run in the north and Scot Run, Transue
Run, Bisbing Run, Bulger's Run, and Cranberry Creek in the mid-section.
Those running north into the Pocono Creek's mid-section are Colmoor Creek
and Reeders Run. Wigwam Run, Flagler Run, Big Meadow and Little Pocono
are within the lower third of the watershed. Sand Spring Run and Wolf
Swamp Run are designated Exceptional Value.
A number of sewage treatment plants discharge into the Pocono and its
tributaries, including: Caesars Brookdale, discharges to Brookdale Lake;
Crossings Outlet Mall, Camelback Ski Resort, Big Pocono Utilities, and
Pocono Auto-Truck Stop discharge to the Pocono; PennDot rest-stop on Rte
80, Fountain Court and Fountain Court West discharge to tributaries; Barton
Court Trailer Park and Monroe County Vo-Tech School discharge to Laurel
Lake Run; Birchwood Resort discharges to the Cranberry Bog.
Evidence indicates that the Pocono Creek watershed is a high-quality
resource on the edge of decline, and that same evidence may reveal the
thresholds at which impairment occurs. Many negative impacts have been
observed in localized areas. The natural resilience of the watershed is
currently taxed by development, transportation, and maintenance practices.
Storm water runoff from parking lots and roads causes habitat damage and
numerous localized stream modifications such as roads, bridges, culverts,
channelized areas, floodplain development, and riparian vegetation removal
degrade the watershed's streams as well.
Big Pocono Mountain (Camelback) forms the watershed divide between the
McMichael and the Pocono watersheds. Camelback ski area, on the north
face of the mountain, drains to the Pocono Creek.
|