Rattling Run | |
---|---|
Rattling Run looking upstream in Gordon | |
Physical characteristics | |
Source | |
• elevation | 1,460 ft (450 m) |
Mouth | |
• location | Little Mahanoy Creek |
• coordinates | 40°45′10″N76°20′22″W / 40.75286°N 76.33935°W Coordinates: 40°45′10″N76°20′22″W / 40.75286°N 76.33935°W |
• elevation | 810 ft (250 m) |
Length | 2.3 mi (3.7 km) |
Basin size | 2.75 sq mi (7.1 km2) |
Basin features | |
Progression | Little Mahanoy Creek → Mahanoy Creek → Susquehanna River → Chesapeake Bay |
Rattling Run is a tributary of Little Mahanoy Creek in Schuylkill County, Pennsylvania, in the United States. It is approximately 2.3 miles (3.7 km) long and flows through Butler Township and Gordon. [1] The watershed of the stream has an area of 2.75 square miles (7.1 km2). The stream is not designated as an impaired waterbody and is several miles from the Western Middle Anthracite Field. The Gordon Reservoir is located within its watershed. The watershed of Rattling Run is a Coldwater Fishery and a Migratory Fishery.
Rattling Run begins on a mountain in Butler Township. It flows west-southwest for a few tenths of a mile before turning northwest and flowing through the Gordon Reservoir. The stream then turns west-southwest for several tenths of a mile, entering a valley and flowing alongside Highridge Park Road/Gordon Mountain Road. It then turns northwest for several tenths of a mile before turning north-northwest and entering Gordon. Here, it leaves its valley and continues flowing north-northwest. After a few tenths of a mile, it reaches its confluence with Little Mahanoy Creek. [1]
Rattling Run joins Little Mahanoy Creek 0.32 miles (0.51 km) upstream of its mouth. [2]
Rattling Run is not designated as an impaired waterbody. [3] In general, the mouth of Rattling Run was found to have a slightly lower pH and slightly lower nutrient concentrations than Little Mahanoy Creek. [4]
The discharge of Rattling Run was measured to be 9.61 cubic feet per second (0.272 m3/s) in March 2001 and 1.99 cubic feet per second (0.056 m3/s) in August 2001. The concentrations of dissolved oxygen were 12.3 and 8.3 milligrams per liter (0.0123 and 0.0083 oz/cu ft), respectively. In March 2001, the pH of the stream was 5.7 and the net alkalinity concentration was 3 milligrams per liter (0.0030 oz/cu ft), while in August 2001, the pH was 6.5. [4]
The concentration of dissolved aluminum in Rattling Run was 0.14 milligrams per liter (0.00014 oz/cu ft) in March 2001 and 0.01 milligrams per liter (1.00×10−5 oz/cu ft). The concentrations of dissolved manganese and iron in the stream were 0.09 and 0.01 milligrams per liter (8.99×10−5 and 1.00×10−5 oz/cu ft) in March 2001 and 0.01 and 0.01 milligrams per liter (1.00×10−5 and 1.00×10−5 oz/cu ft) in August 2001. [4]
The dissolved nitrate concentration in Rattling Run was 0.10 milligrams per liter (0.000100 oz/cu ft) in March 2001 and 0.18 milligrams per liter (0.00018 oz/cu ft) in August 2001. The dissolved phosphorus concentration was 0.03 milligrams per liter (3.0×10−5 oz/cu ft) in March and less than 0.01 milligrams per liter (1.00×10−5 oz/cu ft) in August. The dissolved sulfate concentration was 7 and 6 milligrams per liter (0.0070 and 0.0060 oz/cu ft) in March and August 2001, respectively. [4]
The elevation near the mouth of Rattling Run is 810 feet (250 m) above sea level. [5] The elevation of the stream's source is 1,460 feet (450 m) above sea level. [1]
Rattling Run is a few miles to the south of the Western Middle Anthracite Field. [4] The stream has experienced some erosion along the sides and bottom of its channel. [6]
The watershed of Rattling Run has an area of 2.75 square miles (7.1 km2). [2] The mouth of the stream is in the United States Geological Survey quadrangle of Ashland. However, its source is in the quadrangle of Minersville. [5]
A reservoir known as the Gordon Reservoir is on Rattling Run. In 1970, it was owned by the Butler Township Water Company. [7]
The designated use for Rattling Run is aquatic life. [3]
Rattling Run flooded during Hurricane Agnes in April 1972, causing $350,000 in damage and significant damage to nearby structures. [6] [8]
Rattling Run was entered into the Geographic Names Information System on August 2, 1979. Its identifier in the Geographic Names Information System is 1184693. [5]
Rattling Run was stocked with 1000 adult and yearling rainbow trout at least once in the early 1900s. [9] Improvements were made to the stream in 1937. [10] Flood control proposals for Rattling Run in Gordon were made in 1976. [6]
A steel culvert bridge carrying Gordon Mountain Road over Rattling Run was built in 1959 and is 24.0 feet (7.3 m) long. [11]
In June 1991, it was reported that raw sewage was being piped from homes directly into Rattling Run and Little Mahanoy Creek. [12]
In 2001, neither fish nor macroinvertebrates were observed in Rattling Run at Gordon. [4] The stream is classified as a Coldwater Fishery and a Migratory Fishery. [13]
Shamokin Creek is a tributary of the Susquehanna River in Northumberland County, Pennsylvania, in the United States. It is approximately 32.4 miles (52.1 km) long and flows through Mount Carmel, Mount Carmel Township, Coal Township, Shamokin, Ralpho Township, Shamokin Township, Snydertown, Upper Augusta Township, and Sunbury. The watershed of the creek has an area of 137 square miles (350 km2). It experiences significant impacts by abandoned mine drainage and many abandoned mine drainage discharges are in its watershed. Various other impairments also affect parts of the creek's watershed. Shamokin Creek is in the Appalachian Mountains section of the Ridge and Valley physiographic province. Rock formations consisting of sandstone, shale, and anthracite deposits occur in the watershed.
Mahanoy Creek is a 51.6-mile-long (83.0 km) tributary of the Susquehanna River in Northumberland and Schuylkill counties, Pennsylvania. There are at least 35 sources of acid mine drainage in the creek's watershed. Anthracite was mined in the upper part of the Mahanoy Creek watershed in the 19th and 20th centuries. Mahanoy Creek's tributaries include Schwaben Creek, Zerbe Run, Little Mahanoy Creek, Shenandoah Creek, and North Mahanoy Creek. Little Mahanoy Creek and Schwaben Creek are two streams in the watershed that are unaffected by acid mine drainage. Schwaben Creek has a higher number and diversity of fish species than the main stem.
Little Mahanoy Creek is a 7.5 miles (12.1 km) tributary of Mahanoy Creek in Schuylkill County, Pennsylvania. It starts in the borough of Frackville and joins Mahanoy Creek in the borough of Gordon. Its one named tributary is Rattling Run. The creek's watershed has an area of 11.6 square miles (30 km2). Its watershed is not affected by mining. Compounds found in the waters of the creek include nitrogen, phosphorus, orthophosphates, phosphates, nitrates, and ammonia.
Rattling Run is a tributary of Catawissa Creek in Schuylkill County, Pennsylvania, in the United States. It is approximately 2.4 miles (3.9 km) long and flows through East Union Township. The watershed of the stream has an area of 2.28 square miles (5.9 km2). The stream is considered to be a High-Quality Coldwater Fishery and Class A Wild Trout Waters. Three species of fish inhabit the stream. The main rock formations in the stream's watershed are the Mauch Chunk Formation and the Pottsville Formation and the main soils are the Leck Kill soil and the Hezleton soil. The stream has two unnamed tributaries.
Millers Run is a tributary of Shamokin Creek in Northumberland County, Pennsylvania, in the United States. It is approximately 4.1 miles (6.6 km) long and flows through Ralpho Township. The watershed of the stream has an area of 5.48 square miles (14.2 km2). The stream is not impacted by mining and is not designated as an impaired waterbody. It is a small stream near the lower Shamokin Creek watershed. A number of bridges have been constructed over it. The watershed of Millers Run is designated as a Coldwater Fishery and a Migratory Fishery.
Furnace Run is a tributary of Shamokin Creek in Northumberland County, Pennsylvania, in the United States. It is approximately 1.0 mile (1.6 km) long and flows through Coal Township and Shamokin. The watershed of the stream has an area of 1.61 square miles (4.2 km2). It is impaired by sedimentation and siltation from urban runoff and storm sewers, but is not impacted by mine drainage. Reaches of the stream have been entirely enclosed. Furnace Run is named after a furnace that was built in the area in 1825. The stream is designated as a Coldwater Fishery and a Migratory Fishery.
Carbon Run is a tributary of Shamokin Creek in Northumberland County, Pennsylvania, in the United States. It is approximately 5.2 miles (8.4 km) long and flows through Zerbe Township, Coal Township, and Shamokin. The watershed of the stream has an area of 8.78 square miles (22.7 km2). Carbon Run is impaired due to metals from acid mine drainage, which colors the stream orange. Metals such as manganese, iron, aluminum, and others occur within its water. The watershed of the stream is in the Coal Region of Pennsylvania. Much of the area in the vicinity of the stream consists of spoil piles and abandoned mining land.
Coal Run is a tributary of Shamokin Creek in Northumberland County, Pennsylvania, in the United States. It is approximately 4.7 miles (7.6 km) long and flows through Mount Carmel Township, Coal Township, and Shamokin. The watershed of the stream has an area of 6.25 square miles (16.2 km2). The stream is designated as an impaired waterbody due to metals from abandoned mine drainage. It is an ephemeral stream. Virtually all of the watershed is in coal mining regions.
Quaker Run is a tributary of Shamokin Creek in Northumberland County, Pennsylvania, in the United States. It is approximately 3.7 miles (6.0 km) long and flows through Kulpmont, Mount Carmel Township, and Coal Township. The watershed of the stream has an area of 3.62 square miles (9.4 km2). The stream has one unnamed tributary. Quaker Run is designated as an impaired waterbody due to metals from abandoned mine drainage. Raw sewage and stormwater have also been discharged into it at times.
Locust Creek is a tributary of Shamokin Creek in Northumberland County, Pennsylvania, in the United States. It is approximately 4.0 miles (6.4 km) long and flows through East Cameron Township and Mount Carmel Township. The watershed of the creek has an area of 5.75 square miles (14.9 km2). The stream is designated as impaired due to metals from abandoned mine drainage. It also experiences a low pH. The creek flows through a water gap in Locust Mountain. Prominent land uses in its watershed include refuse areas and forested land. The creek's watershed is designated as a Coldwater Fishery and a Migratory Fishery.
North Branch Shamokin Creek is a tributary of Shamokin Creek in Columbia County and Northumberland County, Pennsylvania, United States. It is approximately 4.8 miles (7.7 km) long and flows through Conyngham Township in Columbia County and Mount Carmel Township in Northumberland County. The watershed of the creek has an area of 5.73 square miles (14.8 km2). The entirety of the creek is designated as an impaired waterbody due to metals from abandoned mine drainage. It is acidic, but its pH has been increasing. Underground mine complexes occur within the watershed. The creek has a permeable streambed and experiences flow loss.
Mouse Creek is a tributary of Schwaben Creek in Northumberland County, Pennsylvania, in the United States. It is approximately 5.6 miles (9.0 km) long and flows through Jordan Township, Washington Township, and Jackson Township. The watershed of the creek has an area of 7.19 square miles (18.6 km2). The creek and its tributaries are not designated as impaired waterbodies. Its watershed is at least partially in the ridge and valley physiographic province. The main land use in the upper reaches of the creek's drainage basin are forested land and agricultural land, but other land uses exist as well. A number of bridges have been constructed across the creek.
Middle Creek is a tributary of Schwaben Creek in Northumberland County, Pennsylvania, in the United States. It is approximately 3.5 miles (5.6 km) long and flows through Washington Township. The watershed of the creek has an area of 3.28 square miles (8.5 km2). The creek is designated as an impaired waterbody, with the cause of the impairment being siltation, low dissolved oxygen levels/organic enrichment, and vegetation removal and the source being agricultural activity. The creek is classified as a Trout Stocked Fishery.
Zerbe Run is a tributary of Mahanoy Creek in Northumberland County, Pennsylvania, in the United States. It is approximately 8.3 miles (13.4 km) long and flows through Coal Township, Zerbe Township, and Little Mahanoy Township. The watershed of the stream has an area of 13.1 square miles (34 km2). Part of the stream is impaired by abandoned mine drainage, but its upper reaches are not impacted by mining. Several mine drainage discharges occur within the watershed. The stream is not far from the Western Middle Anthracite Field.
Crab Run is a tributary of Mahanoy Creek in Schuylkill County, Pennsylvania, in the United States. It is approximately 2.5 miles (4.0 km) long and flows through Barry Township. The watershed of the stream has an area of 3.50 square miles (9.1 km2). Despite being listed as impaired by abandoned mine drainage, the stream is not impacted by this; no mining has been done in its watershed. However, some stream reaches in its watershed do experience agricultural impacts. The stream is not far from the Western Middle Anthracite Field. Its watershed is designated as a Coldwater Fishery and a Migratory Fishery. As of 2001, the stream contains macroinvertebrates, but no fish.
Lost Creek is a tributary of Shenandoah Creek in Schuylkill County, Pennsylvania, in the United States. It is approximately 1.3 miles (2.1 km) long and flows through West Mahanoy Township. The watershed of the creek has an area of 1.32 square miles (3.4 km2). The creek is an ephemeral stream in its lower reaches and is impaired by abandoned mine drainage. It is in the Western Middle Anthracite Field. The creek has historically been used as a water supply. It is designated as a Coldwater Fishery.
North Mahanoy Creek is a tributary of Mahanoy Creek in Schuylkill County, Pennsylvania, in the United States. It is approximately 4.4 miles (7.1 km) long and flows through Delano Township, Mahanoy Township, and Mahanoy City. The watershed of the creek has an area of 5.99 square miles (15.5 km2). The creek is designated as an impaired waterbody due to sedimentation/siltation and water/flow variation from abandoned mine drainage. The creek is relatively small, an ephemeral stream in its lower reaches, and is located within the Western Middle Anthracite Field.
Kehly Run is a tributary of Shenandoah Creek in Schuylkill County, Pennsylvania, in the United States. It is less than 2 miles (3.2 km) long and flows through West Mahanoy Township and possibly Shenandoah. The watershed of the stream has an area of 1.63 square miles (4.2 km2). The stream is located within the Western Middle Anthracite Field. A number of dams have been constructed across it. The stream is classified as a Coldwater Fishery and has macroinvertebrates, but no fish.
Fidlers Run is a tributary of the Susquehanna River in Northumberland County, Pennsylvania, in the United States. It is approximately 3.1 miles (5.0 km) long and flows through Jackson Township and Lower Mahanoy Township. The watershed of the stream has an area of 6.88 square miles (17.8 km2). The stream is not designated as an impaired waterbody, although a reaches of a few of its unnamed tributaries are. It is a small stream, with a width of 3 to 5 feet. Large areas of agricultural land occur along a substantial portion of its length.
Hans Yost Creek is a tributary of Deep Creek in Schuylkill County, Pennsylvania, in the United States. It is approximately 3.4 miles (5.5 km) long and flows through Foster Township and Barry Township. The watershed of the creek has an area of 3.52 square miles (9.1 km2). The creek is designated as an impaired waterbody, with the causes being metals and pH and the probable source being abandoned mine drainage. It has no named tributaries, but two abandoned mine discharges flow into it. The creek's watershed was extensively mined in the late 1800s and early 1900s, but the only remaining active mining permits are for remining.