Swanks Run | |
---|---|
Location | |
Physical characteristics | |
Source | |
⁃ location | plateau in Davidson Township, Sullivan County, Pennsylvania |
⁃ elevation | between 2,240 and 2,260 feet (680 and 690 m) |
Mouth | |
⁃ location | West Branch Fishing Creek in Davidson Township, Sullivan County, Pennsylvania |
⁃ coordinates | 41°19′08″N76°31′23″W / 41.3188°N 76.5231°W Coordinates: 41°19′08″N76°31′23″W / 41.3188°N 76.5231°W |
⁃ elevation | 1,978 ft (603 m) |
Length | 1.5 mi (2.4 km) |
Basin size | 1.33 sq mi (3.4 km2) |
Basin features | |
Progression | West Branch Fishing Creek → Fishing Creek → Susquehanna River → Chesapeake Bay |
Tributaries | |
⁃ left | one unnamed tributary |
Swanks Run is a tributary of West Branch Fishing Creek in Sullivan County, Pennsylvania, in the United States. It is approximately 1.5 miles (2.4 km) long and flows through Davidson Township. [1] The watershed of the stream has an area of 1.33 square miles (3.4 km2). The stream is considered to be Class A Wild Trout Waters for its entire length. Boulder Colluvium, alluvium, and bedrock consisting of sandstone and shale can be found in the vicinity of the stream. It is on Pennsylvania State Game Lands.
Swanks Run begins on a plateau in Davidson Township. It flows east for several tenths of a mile, entering a small and narrow valley. It then receives an unnamed tributary from the left and turns southeast. Its valley becomes deeper as it flows downstream. After several tenths of a mile, the stream reaches its confluence with West Branch Fishing Creek. [1]
Swanks Run joins West Branch Fishing Creek 10.64 miles (17.12 km) upstream of its mouth. [2]
Swanks Run has no named tributaries. However, it does have one unnamed tributary, which is slightly less than half a mile long and flows in a north-to-south direction. [1]
The concentration of alkalinity in the waters of Swanks Run is one milligram per liter. [3]
The elevation near the mouth of Swanks Run is 1,978 feet (603 m) above sea level. [4] The elevation of the stream's source is between 2,240 and 2,260 feet (680 and 690 m) above sea level. [1]
Swanks Run is on bedrock consisting of sandstone and shale for nearly its entire length. However, near the mouth of the stream, there is alluvium containing stratified silt, sand, and gravel, as well as some boulders. Additionally, a colluvium known as Boulder Colluvium occurs near the stream's mouth and also in the higher portions of the watershed, above the stream's valley. In these areas, the majority of the surface is covered in boulders and cobbles consisting of quartz, sandstone, or conglomerate. [5]
The watershed of Swanks Run has an area of 1.33 square miles (3.4 km2). [2] The stream is entirely within the United States Geological Survey quadrangle of Sonestown. [4]
Swanks Run is on public and open land for its entire length. [3] The stream is in the western part of Pennsylvania State Game Lands Number 13. [6]
Swanks Run was entered into the Geographical Names Information System on August 2, 1979. Its identifier in the Geographical Names Information System is 1189137. [4]
Swanks Run is considered by the Pennsylvania Fish and Boat Commission to be Class A Wild Trout Waters for brook trout. The stream holds this designation between its headwaters and its mouth. It is one of six streams to be designated as Class A Wild Trout Waters in Sullivan County. [3]
Wasp Branch is a tributary of Pine Creek in Luzerne County, Pennsylvania, in the United States. It is approximately 1.7 miles (2.7 km) long and flows through Fairmount Township. The watershed of the stream has an area of 0.90 square miles (2.3 km2). The stream is considered to be Class A Wild Trout Waters, a Coldwater Fishery, and a Migratory Fishery. Glacial till and bedrock consisting of stone and shale can be found in the stream's vicinity.
Chimneystack Run is a tributary of Coles Creek in Columbia County, Pennsylvania, in the United States. It is approximately 1.8 miles (2.9 km) long and flows through Sugarloaf Township. The watershed of the stream has an area of 1.07 square miles (2.8 km2). The stream's headwaters are located between Red Rock Mountain and Central Mountain. It has no named tributaries, but one unnamed tributary. Chimneystack Run is named after Chimneystack Rock. Wild trout inhabit the stream. Glaciation has affected the geography and geology in its vicinity.
Elk Run is tributary of West Branch Fishing Creek in Sullivan County and Columbia County, in Pennsylvania, in the United States. It is approximately 4.8 miles (7.7 km) long and flows through Davidson Township in Sullivan County and Sugarloaf Township in Columbia County. The watershed of the stream has an area of 7.49 square miles (19.4 km2). The stream has three named tributaries: Gallows Run, Hog Run, and Long Run. Elk Run is considered to be an Exceptional Value stream and a Migratory Fishery. The forests surrounding it are deemed by the Sullivan County Natural Areas Inventory to be a "locally significant" area. The stream is named for an elk that was killed in it in the 1840s.
Painter Run is a tributary of West Branch Fishing Creek in Sullivan County, Pennsylvania, in the United States. It is approximately 4.5 miles (7.2 km) long and flows through Davidson Township. The watershed of the stream has an area of 5.20 square miles (13.5 km2). It has one named tributary, which is known as Oxhorn Run and one unnamed tributary. Painter Run is slightly acidic, with pH values ranging from 5.99 to 6.88. The stream is in a narrow valley with several ridges nearby. Sandstone of the Pocono Formation occurs near it. At least two bridges have been constructed over the stream. Its unnamed tributary is considered to be Class A Wild Trout Waters.
Shingle Mill Run is a tributary of West Branch Fishing Creek in Sullivan County, Pennsylvania, in the United States. It is approximately 2.4 miles (3.9 km) long and flows through Davidson Township. The watershed of the stream has an area of 2.60 square miles (6.7 km2). The stream has one named tributary, Bearwallow Run. Shingle Mill Run is designated as an Exceptional Value stream and has a population of native trout. The stream has high water quality and is slightly acidic. Boulder Colluvium and bedrock consisting of sandstone and shale can be found near the stream.
Laurel Run is a tributary of West Branch Fishing Creek in Sullivan County, Pennsylvania, in the United States. It is approximately 1.2 miles (1.9 km) long and flows through Davidson Township. The stream is in the United States Geological Survey quadrangle of Elk Grove. Wisconsinan Flow-Till, Boulder Colluvium, Wisconsinan Till Moraine, alluvium, and alluvial fan occur in the vicinity of the stream, as does bedrock consisting of sandstone and shale. The southern terminus of the late Wisconsinan glaciation is also in the area. A wood plank bridge on stone masonry abutment walls crosses the stream.
Deep Hollow is a tributary of West Branch Fishing Creek in Luzerne County, Pennsylvania, in the United States. It is approximately 0.8 miles (1.3 km) long and flows through Davidson Township. The watershed of the stream has an area of 0.53 square miles (1.4 km2). Wild trout naturally reproduce in the stream. The surficial geology in the area mainly features bedrock consisting of sandstone and shale, as well as a small amount of Boulder Colluvium and alluvium.
Spencer Run is a tributary of West Creek in Columbia County, Pennsylvania, in the United States. It is approximately 2.1 miles (3.4 km) long and flows through Jackson Township and Benton Township. The watershed of the stream has an area of 2.07 square miles (5.4 km2). Wild trout naturally reproduce in the stream. The surficial geology in the area mainly features Illinoian Till, Illinoian Leg, alluvium, colluvium, and bedrock.
York Hollow is a tributary of West Creek in Columbia County, Pennsylvania, in the United States. It is approximately 2.5 miles (4.0 km) long and flows through Jackson Township and Sugarloaf Township. The watershed of the stream has an area of 1.47 square miles (3.8 km2). Wild trout naturally reproduce in the stream. The surficial geology in the area mainly consists of Illinoian Till, Illinoian Lag, alluvium, colluvium, and bedrock.
Bearwallow Run is a tributary of Shingle Mill Run in Sullivan County, Pennsylvania, in the United States. It is approximately 1.3 miles (2.1 km) long and flows through Davidson Township, Sullivan County, Pennsylvania. The watershed of the stream has an area of 1.02 square miles (2.6 km2). The stream is considered to be Class B Wild Trout Waters and wild trout reproduce naturally within it. The surficial geology in the area mainly consists of bedrock and Boulder Colluvium.
Slip Run is a tributary of West Branch Fishing Creek in Sullivan County, Pennsylvania, in the United States. It is approximately 1.1 miles (1.8 km) long and flows through Davidson Township. The watershed of the stream has an area of 0.53 square miles (1.4 km2). Wild trout naturally reproduce within the stream. Surficial geology in the area mainly consists of alluvium, Boulder Colluvium, Wisconsinan Till Moraine, Wisconsinan Till, and bedrock consisting of sandstone and shale.
Karnes Hollow is a tributary of Fishing Creek in Columbia County, Pennsylvania, in the United States. It is approximately 1.1 miles (1.8 km) long and flows through Fishing Creek Township and Benton Township. The watershed of the stream has an area of 0.90 square miles (2.3 km2). The stream is named after a valley whose etymology is unknown. The surficial geology in its vicinity consists of colluvium, alluvium, Illinoian Till, Illinoian Lag, and bedrock consisting of sandstone and shale.
Plank Bridge Creek is a tributary of Spring Brook in Lackawanna County, Pennsylvania, in the United States. It is approximately 2.4 miles (3.9 km) long and flows through Spring Brook Township. The watershed of the creek has an area of 1.26 square miles (3.3 km2). It is inhabited by wild trout throughout its length. The surficial geology in its vicinity mainly consists of Wisconsinan Till, bedrock, Boulder Colluvium, alluvium, and wetlands.
Kellum Creek is a tributary of Roaring Brook in Lackawanna County, Pennsylvania, in the United States. It is approximately 2.9 miles (4.7 km) long and flows through Madison Township. The watershed of the creek has an area of 2.56 square miles (6.6 km2). The creek is considered to be Class A Wild Trout Waters. A planned trail is in its vicinity. The surficial geology in the area consists of alluvium, bedrock, peat bogs, wetlands, Boulder Colluvium, and Wisconsinan Till.
Lake Run is a tributary of Roaring Brook in Lackawanna County, Pennsylvania, in the United States. It is approximately 1.6 miles (2.6 km) long and flows through Covington Township. The watershed of the stream has an area of 3.44 square miles (8.9 km2). It has one named tributary, which is known as Emerson Run. Lake Run is considered to be Class A Wild Trout Waters. The surficial geology in its vicinity consists of Wisconsinan Ice-Contact Stratified Drift, Wisconsinan Till, Boulder Colluvium, alluvium, bedrock, sand and gravel pits, fill, wetlands, peat bogs, and a lake.
Roaring Run is a tributary of Bowman Creek in Wyoming County, Pennsylvania, in the United States. It is approximately 4.9 miles (7.9 km) long and flows through Forkston Township, Noxen Township, and Monroe Township. It has two named tributaries: Newton Run and South Branch Roaring Run. The watershed of Roaring Run has an area of 11.4 square miles (30 km2). It is designated as a High-Quality Coldwater Fishery and a Migratory Fishery and the stream is Class A Wild Trout Waters. The surficial geology in its vicinity consists of alluvium, alluvial terrace, alluvial fan, bedrock, Wisconsinan Till, and Wisconsinan Ice-Contact Stratified Drift. A bridge carrying Pennsylvania Route 29 crosses the stream.
South Branch Bowman Creek is a tributary of Bowman Creek in Luzerne County, Pennsylvania, in the United States. It is approximately 3.0 miles (4.8 km) long and flows through Fairmount Township and Ross Township. The watershed of the creek has an area of 3.92 square miles (10.2 km2). The surficial geology in its vicinity consists of alluvial fan, alluvium, Wisconsinan Ice-Contact Sratified Drift, fill, lakes, Boulder Colluvium, Wisconsinan Till, Wisconsinan Bouldery Till, wetlands, and bedrock. Most of the creek is in Ricketts Glen State Park. It has one named tributary, which is known as Cherry Run. The creek's watershed is designated as a High-Quality Coldwater Fishery and a Migratory Fishery.
Buck Run is a tributary of Little Muncy Creek in Lycoming County, Pennsylvania, in the United States. It is approximately 1.3 miles (2.1 km) long and flows through Jordan Township. The watershed of the stream has an area of 0.81 square miles (2.1 km2). The surficial geology near the stream mostly consists of Illinoian Till and Illinoian Lag, with some alluvium and bedrock. The stream is a Coldwater Fishery and is being considered for wild trout designation. It has one unnamed tributary.
West Branch Little Muncy Creek is a tributary of Little Muncy Creek in Sullivan County and Lycoming County, in Pennsylvania, in the United States. It is approximately 3.5 miles (5.6 km) long and flows through Davidson Township in Sullivan County and Franklin Township and Jordan Township in Lycoming County. The watershed of the creek has an area of 4.33 square miles (11.2 km2). The creek has one named tributary, which is known as West Creek. The surficial geology in the vicinity of West Branch Little Muncy Creek includes alluvium, bedrock, fill, Wisconsinan and Reworked Illinoian Till, Wisconsinan Till, Wisconsinan Flow-Till, Wisconsinan Till Moraine, and Boulder Colluvium. The creek designated as a Coldwater Fishery and a Migratory Fishery and is being considered for addition to the wild trout waters list of the Pennsylvania Fish and Boat Commission.
Little Indian Run is a tributary of Little Muncy Creek in Lycoming County and Sullivan County, in Pennsylvania, in the United States. It is approximately 4.3 miles (6.9 km) long and flows through Franklin Township and Jordan Township in Lycoming County and Davidson Township in Sullivan County. The watershed of the stream has an area of 3.36 square miles (8.7 km2). The surficial geology in the stream's vicinity mainly consists of alluvium, bedrock, Wisconsinan Till, Wisconsinan Till Moraine, and Wisconsinan Ice-Contact Stratified Drift. Wild trout naturally reproduce within the stream. A number of sawmills were historically located on the stream.