Rock Bottom Creek

Last updated
Rock Bottom Creek
Physical characteristics
Main source lake in Jefferson Township, Lackawanna County, Pennsylvania
between 1,720 and 1,740 feet (520 and 530 m)
River mouth Roaring Brook in Roaring Brook Township, Lackawanna County, Pennsylvania
1,306 ft (398 m)
41°23′23″N75°33′14″W / 41.3898°N 75.5540°W / 41.3898; -75.5540 Coordinates: 41°23′23″N75°33′14″W / 41.3898°N 75.5540°W / 41.3898; -75.5540
Length 3.2 mi (5.1 km)
Basin features
Progression Roaring Brook → Lackawanna RiverSusquehanna RiverChesapeake Bay
Basin size 3.06 sq mi (7.9 km2)

Rock Bottom Creek is a tributary of Roaring Brook in Lackawanna County, Pennsylvania, in the United States. It is approximately 3.2 miles (5.1 km) long and flows through Jefferson Township and Roaring Brook Township. [1] The watershed of the creek has an area of 3.06 square miles (7.9 km2). Wild trout naturally reproduce within it. The surficial geology in the creek's vicinity consists of Wisconsinan Till, alluvium, bedrock, fill, peat bogs, lakes, and wetlands.

Tributary stream or river that flows into a main stem river or lake

A tributary or affluent is a stream or river that flows into a larger stream or main stem river or a lake. A tributary does not flow directly into a sea or ocean. Tributaries and the main stem river drain the surrounding drainage basin of its surface water and groundwater, leading the water out into an ocean.

Lackawanna County, Pennsylvania County in Pennsylvania, United States

Lackawanna County is a county in the U.S. state of Pennsylvania. As of the 2010 census, the population was 214,437. Its county seat and largest city is Scranton.

Jefferson Township, Lackawanna County, Pennsylvania Place in Pennsylvania, United States

Jefferson Township is a township in Lackawanna County, Pennsylvania, United States. The population was 3,731 at the 2010 census.

Contents

Course

Rock Bottom Creek begins in a lake in Jefferson Township. It flows south-southwest for several tenths of a mile before turning northwest and then southwest. After several tenths of a mile, it turns west-northwest, entering Roaring Brook Township and reaching Interstate 84 and flowing southwest in its median strip for several tenths of a mile. The creek then turns west and leaves behind the median strip. A short distance further downstream, it crosses Pennsylvania Route 435 and reaches its confluence with Roaring Brook. [1]

Interstate 84 (I-84) is an Interstate Highway in the northeastern United States that extends from Dunmore, Pennsylvania, at an interchange with I-81 east to Sturbridge, Massachusetts, at an interchange with the Massachusetts Turnpike (I-90). Among the major cities that the road passes through is Hartford, Connecticut. I-84 has distance-based exit numbering in Pennsylvania. Otherwise, exit numbers are roughly sequential. Another highway named I-84 is located in the northwestern United States.

Median strip the reserved area that separates opposing lanes of traffic on divided roadways

The median strip or central reservation is the reserved area that separates opposing lanes of traffic on divided roadways, such as divided highways, dual carriageways, freeways, and motorways. The term also applies to divided roadways other than highways, such as some major streets in urban or suburban areas. The reserved area may simply be paved, but commonly it is adapted to other functions; for example, it may accommodate decorative landscaping, trees, a median barrier or railway, rapid transit, light rail or streetcar lines.

Pennsylvania Route 435 highway in Pennsylvania

Pennsylvania Route 435 (PA 435) is a 14.9-mile-long (24.0 km) state highway located in Monroe, Wayne, and Lackawanna Counties in Pennsylvania. The southern terminus is at Interstate 380 (I-380) near Gouldsboro. The northern terminus is at I-84 and I-380 in Dunmore. The route heads north from I-380 and the southern terminus of PA 507 in Monroe County as a four-lane road, passing through a small section of Wayne County before entering Lackawanna County. PA 435 becomes a two-lane road at the PA 307 junction and continues north to intersect PA 502 in Daleville and PA 690 in Moscow. After intersecting PA 590, the route becomes a four-lane divided highway and intersects PA 348 before merging into I-84/I-380.

Rock Bottom Creek joins Roaring Brook 9.84 miles (15.84 km) upstream of its mouth. [2]

Geography and geology

The elevation near the mouth of Rock Bottom Creek is 1,306 feet (398 m) above sea level. [3] The elevation of the creek's source is between 1,720 and 1,740 feet (520 and 530 m) above sea level. [1]

River mouth end of a river

A river mouth is the part of a river where the river debouches into another river, a lake, a reservoir, a sea, or an ocean.

Sea level Average level for the surface of the ocean at any given geographical position on the planetary surface

Mean sea level (MSL) is an average level of the surface of one or more of Earth's oceans from which heights such as elevation may be measured. MSL is a type of vertical datum – a standardised geodetic datum – that is used, for example, as a chart datum in cartography and marine navigation, or, in aviation, as the standard sea level at which atmospheric pressure is measured to calibrate altitude and, consequently, aircraft flight levels. A common and relatively straightforward mean sea-level standard is the midpoint between a mean low and mean high tide at a particular location.

River source The starting point of a river

The source or headwaters of a river or stream is the furthest place in that river or stream from its estuary or confluence with another river, as measured along the course of the river.

Rock Bottom Glen is in the watershed of Rock Bottom Creek, in Roaring Brook Township. The Muni Bogs are in the watershed in Jefferson Township. [4]

The surficial geology in the vicinity of Rock Bottom Creek mainly consists of a glacial or resedimented till known as Wisconsinan Till. However, there are also large patches of bedrock consisting of congloemratic sandstone, sandstone, and shale. There are smaller patches of wetlands, peat bogs, lakes and fill. There is also an area of alluvium at the mouth of the creek. [5]

Till Unsorted glacial sediment

Till or glacial till is unsorted glacial sediment.

Bedrock Lithified rock under the regolith

In geology, bedrock is the lithified rock that lies under a loose softer material called regolith at the surface of the Earth or other terrestrial planets. The broken and weathered regolith includes soil and subsoil. The surface of the bedrock beneath the soil cover is known as rockhead in engineering geology, and its identification by digging, drilling or geophysical methods is an important task in most civil engineering projects. Superficial deposits can be extremely thick, such that the bedrock lies hundreds of meters below the surface.

Sandstone A clastic sedimentary rock composed mostly of sand-sized particles

Sandstone is a clastic sedimentary rock composed mainly of sand-sized mineral particles or rock fragments.

Watershed and hydrology

The watershed of Rock Bottom Creek has an area of 3.06 square miles (7.9 km2). [2] The creek is entirely within the United States Geological Survey quadrangle of Olyphant. [3]

The Jefferson Township Sewer Authority once applied for a permit to discharge into an unnamed tributary of Rock Bottom Creek. [6]

History

Rock Bottom Creek was entered into the Geographic Names Information System on August 2, 1979. Its identifier in the Geographic Names Information System is 1199396. [3]

In the early 2000s, the Lackawanna River Watershed Conservation Plan recommended that Roaring Brook Township and Jefferson Township include protection of Keyser Creek in their zoning plans. [4]

Biology

Wild trout naturally reproduce in Rock Bottom Creek from its headwaters downstream to its mouth. [7] An unnamed tributary of the creek is considered to be a High-Quality Coldwater Fishery. [6] Rock Bottom Creek was stocked with trout in the early 1900s. [8]

See also

Related Research Articles

Monument Creek is a tributary of Spring Brook in Luzerne County and Lackawanna County, in Pennsylvania, in the United States. It is approximately 2.8 miles (4.5 km) long and flows through Pittston Township in Luzerne County and Spring Brook Township. The creek is considered to be a High-Quality Coldwater Fishery. It has one named tributary, which is known as Trout Creek. The surficial geology in the vicinity of Monument Creek consists of bedrock, Wisconsinan Till, alluvium, Wisconsinan Ice-Contact Stratified Drift, and fill.

Trout Creek is a tributary of Monument Creek in Lackawanna County, Pennsylvania, in the United States. It is approximately 3.4 miles (5.5 km) long and flows through Spring Brook Township. Wild trout naturally reproduce in the creek. It has no named tributaries, but does have three unnamed tributaries. The surficial geology in the vicinity of the creek mainly consists of bedrock, Wisconsinan Till, alluvium, fill, wetlands, and lakes.

Green Run is a tributary of Spring Brook in Lackawanna County, Pennsylvania, in the United States. It is approximately 4.7 miles (7.6 km) long and flows through Spring Brook Township, Roaring Brook Township, and Scranton. The watershed of the stream has an area of 4.32 square miles (11.2 km2). It is considered to be Class A Wild Trout Waters throughout its entire length. Numerous macroinvertebrate taxa also inhabit the stream. The surficial geology in the vicinity of the stream's lower reaches mainly consists of Wisconsinan Till, bedrock, and Boulder Colluvium.

Rattlesnake Creek is a tributary of Spring Brook in Lackawanna County, Pennsylvania, in the United States. It is approximately 5.0 miles (8.0 km) long and flows through Spring Brook Township. The watershed of the creek has an area of 9.18 square miles (23.8 km2). The creek has one named tributary, which is known as Six Springs Creek. Rattlesnake Creek is inhabited by wild trout and part of it is considered to be Class A Wild Trout Waters. A dammed lake known as Maple Lake is located near its headwaters. The surficial geology in the area mainly consists of Wisconsinan Till and bedrock, with some alluvium, Wisconsinan Ice-Contact Stratified Drift, wetlands, and peat bogs.

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.

Panther Creek is a tributary of Spring Brook in Lackawanna County, Pennsylvania, in the United States. It is approximately 2.7 miles (4.3 km) long and flows through Thornhurst Township, Clifton Township, and Spring Brook Township. The watershed of the creek has an area of 7.18 square miles (18.6 km2). It has one named tributary, which is known as Painter Creek. Panther Creek is considered to be Class A Wild Trout Waters. The surficial geology in its vicinity consists of alluvium, alluvial terrace, Wisconsinan Till, and bedrock.

Painter Creek river in the United States of America

Painter Creek is a tributary of Panther Creek in Lackawanna County, Pennsylvania, in the United States. It is approximately 3.4 miles (5.5 km) long and flows through Thornhurst Township and Spring Brook Township. The watershed of the creek has an area of 4.51 square miles (11.7 km2). Wild trout naturally reproduce in the creek and a hiking trail is in its vicinity. The surficial geology in the area consists of Wisconsinan Till, bedrock, and wetlands. A bog known as the Painter Creek Bog is listed on the Lackawanna County Natural Areas Inventory.

Little Roaring Brook is a tributary of Roaring Brook in Lackawanna County, Pennsylvania, in the United States. It is approximately 3.4 miles (5.5 km) long and flows through Olyphant, Throop, and Dunmore. The watershed of the stream has an area of 3.06 square miles (7.9 km2). It contains several watersheds: Dunmore Reservoir Number One, Marshwood Reservoir, and Dunmore Reservoir Number Three. Some strip mining has been done in the stream's vicinity and it has a high load of sediment. The surficial geology in the stream's vicinity consists of Wisconsinan Till, surface mining land, bedrock, urban land, and wetlands.

White Oak Run is a tributary of Roaring Brook in Lackawanna County, Pennsylvania, in the United States. It is approximately 2.3 miles (3.7 km) long and flows through Jefferson Township, Madison Township, and Roaring Brook Township. The watershed of the stream has an area of 3.22 square miles (8.3 km2). The stream flows through the Curtis Reservoir, which is dammed by the Curtis Dam. The surficial geology in the vicinity of the stream's mouth includes alluvium, Wisconsinan Till, and bedrock.

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.

Bear Brook is a tributary of Roaring Brook in Lackawanna County, Pennsylvania, in the United States. It is approximately 3.0 miles (4.8 km) long and flows through Madison Township and Moscow. The watershed of the stream has an area of 2.26 square miles (5.9 km2). Wild trout naturally reproduce within it. The surficial geology in the vicinity of the stream's lower reaches consists of Wisconsinan Till, Wisconsinan Ice-Contact Stratified Drift, bedrock, and alluvium. A bridge carrying Pennsylvania Route 690 crosses the stream.

East Branch Roaring Brook is a tributary of Roaring Brook in Wayne County and Lackawanna County, in Pennsylvania in the United States. It is approximately 3.7 miles (6.0 km) long and flows through Sterling Township in Wayne County and Madison Township and Covington Township in Lackawanna County. The watershed of the stream has an area of 5.90 square miles (15.3 km2). Wild trout naturally reproduce within the stream and many macroinvertebrate taxa inhabit it. The surficial geology in the area consists of Wisconsinan Till, Wisconsinan Ice-Contact Stratified Drift, alluvium, bedrock, fill, sand and gravel pits, and wetlands.

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.

Emerson Run is a tributary of Lake Run in Lackawanna County, Pennsylvania, in the United States. It is approximately 1.8 miles (2.9 km) long and flows through Covington Township. The watershed of the stream has an area of 1.58 square miles (4.1 km2). Wild trout naturally reproduce in the stream. The surficial geology in its vicinity consists of Wisconsinan Ice-Contact Stratified Drift, Wisconsinan Till, bedrock, wetlands, peat bogs, and sand and gravel pits.

Brace Brook is a tributary of the Lackawanna River in Wayne County and Susquehanna County, in Pennsylvania, in the United States. It is approximately 2.9 miles (4.7 km) long and flows through Mount Pleasant Township and Clinton Township in Wayne County and Forest City in Susquehanna County. The watershed of the stream has an area of 2.99 square miles (7.7 km2). The stream is not designated as impaired. It drains a portion of the Moosic Mountains. The surficial geology in its vicinity consists of alluvium, surface mining land, coal dumps, fill, Wisconsinan Till, and bedrock containing sandstone and shale. A reservoir known as the Brace Brook Reservoir is in the watershed. The stream's drainage basin is designated as a Coldwater Fishery and a Migratory Fishery.

Beaver Creek is a tributary of Buttermilk Creek in Lackawanna County and Wyoming County, in Pennsylvania, in the United States. It is approximately 5.5 miles (8.9 km) long and flows through West Abington Township in Lackawanna County and Overfield Township and Falls Township in Wyoming County. The watershed of the creek has an area of 9.81 square miles (25.4 km2) and contains Lake Winola. The creek is not designated as an impaired waterbody. The surficial geology in its vicinity consists of alluvium, Wisconsinan Till, Wisconsinan Outwash, alluvial fan, Wisconsinan Ice-Contact Stratified Drift, Wisconsinan Bouldery Till, wetlands, and peat bogs.

Roaring Run (Bowman Creek tributary) river in the United States of America

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 Roaring Run is a tributary of Roaring Run in Wyoming County, Pennsylvania, in the United States. It is approximately 2.0 miles (3.2 km) long and flows through Noxen Township and Forkston Township. The watershed of the stream has an area of 3.31 square miles (8.6 km2). The surficial geology in its vicinity consists of bedrock, Wisconsinan Till, Wisconsinan Bouldery Till, Wisconsinan Ice-Contact Stratified Drift, and alluvium. South Branch Roaring Run is classified as Class A Wild Trout Waters.

Field Brook

Field Brook is a tributary of Tunkhannock Creek in Susquehanna County and Wyoming County, in Pennsylvania, in the United States. It is approximately 5.8 miles (9.3 km) long and flows through Lathrop Township in Susquehanna County and Nicholson Township in Wyoming County. The watershed of the stream has an area of 7.41 square miles (19.2 km2). The stream has one named tributary, which is known as East Branch Field Brook. The surficial geology in the vicinity of Field Brook consists of alluvium, Wisconsinan Till, alluvial terrace, alluvial fan, bedrock, wetlands, and a lake. The watershed of the stream is designated as a Coldwater Fishery and a Migratory Fishery.

Nine Partners Creek is a tributary of Tunkhannock Creek in Susquehanna County, Pennsylvania, in the United States. It is approximately 10 miles (16 km) long and flows through New Milford Township, Harford Township, and Lenox Township. The watershed of the creek has an area of 38.6 square miles (100 km2). The creek has two named tributaries: Butler Creek and Leslie Creek. The surficial geology in the vicinity of Nine Partners Creek includes Wisconsinan Till, alluvium, bedrock, alluvial fan, and wetlands. The creek's drainage basin is designated as a Coldwater Fishery and a Migratory Fishery.

References

  1. 1 2 3 United States Geological Survey, The National Map Viewer , retrieved April 8, 2015
  2. 1 2 Pennsylvania Gazetteer of Streams (PDF), November 2, 2001, retrieved April 9, 2015
  3. 1 2 3 Geographic Names Information System, Feature Detail Report for: Rock Bottom Creek , retrieved April 9, 2015
  4. 1 2 Lackawanna River Corridor Association (2001), Lackawanna River Watershed Conservation Plan (PDF), pp. 63, 66, 115, 120, retrieved April 10, 2015
  5. Duane D. Braun (2006), Surficial geology of the Olyphant 7.5-minute quadrangle, Lackawanna County, Pennsylvania, p. 14, retrieved April 10, 2015
  6. 1 2 "NPDES Stormwater Individual Permit", Pennsylvania Bulletin , retrieved April 10, 2015
  7. Pennsylvania Fish and Boat Commission (January 2015), Pennsylvania Wild Trout Waters (Natural Reproduction) - Jan 2015 (PDF), p. 46, retrieved April 9, 2015
  8. "Streams to Be Stocked", The Scranton Republican , p. 7, March 14, 1914, retrieved April 10, 2015