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Coal Creek (Susquehanna River tributary)

Rivers of Luzerne County, PennsylvaniaRivers of PennsylvaniaTributaries of the Susquehanna River
Coal Creek
Coal Creek

Coal Creek is a tributary of the Susquehanna River in Luzerne County, Pennsylvania, in the United States. It is approximately 2.9 miles (4.7 km) long and flows through Plymouth Township and Plymouth. The watershed of the creek has an area of 1.46 square miles (3.8 km2). A reservoir known as Spring Brook Reservoir Number Four is situated on the creek. The surficial geology near the creek includes Wisconsinan Till, Wisconsinan Ice-Contact Stratified Drift, alluvium, coal dumps, and bedrock consisting of sandstone and shale. On July 3, 2011, Coal Creek flooded when 5 inches (13 cm) of rain fell in the watershed in less than 90 minutes. The flood caused $5 million in damage. The creek is designated as a Coldwater Fishery and a Migratory Fishery.

Excerpt from the Wikipedia article Coal Creek (Susquehanna River tributary) (License: CC BY-SA 3.0, Authors, Images).

Coal Creek (Susquehanna River tributary)
Susquehanna Warrior Trail, Plymouth Township

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Geographical coordinates (GPS)

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N 41.2293 ° E -75.9564 °
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Susquehanna Warrior Trail

Susquehanna Warrior Trail
18651 Plymouth Township
Pennsylvania, United States
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Coal Creek
Coal Creek
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Nanticoke Creek
Nanticoke Creek

Nanticoke Creek is a tributary of the Susquehanna River in Luzerne County, Pennsylvania, in the United States. It is approximately 4.4 miles (7.1 km) long and flows through Hanover Township and Nanticoke. The watershed of the creek has an area of 7.57 square miles (19.6 km2). The creek has one named tributary, which is known as Espy Run. Nanticoke Creek impaired by pH and metals due to abandoned mine drainage. Abandoned mine drainage discharges in the creek's watershed include the Truesdale Mine Discharge and the Askam Borehole. The creek is located in the Northern Middle Anthracite Field and is in the Anthracite Valley Section of the ridge and valley physiographic province. The main rock formations in the watershed include the Mauch Chunk Formation, the Pottsville Group, and the Llewellyn Formation. The surficial geology consists of coal dumps, surface mining land, alluvium, Wisconsinan Outwash, Wisconsinan Till, urban land, and bedrock. The watershed of Nanticoke Creek is mainly forested, but urban land and mining land are also present. The city of Nanticoke is partially in the watershed and many unincorporated communities are there as well. The creek is named after the Nanticoke tribe, but was historically known as Muddy Run before appearing on maps with its present name by 1776. Extensive mining, both underground and on the surface, has been done in the creek's watershed. Numerous passive and active treatment systems have been installed in the watershed in recent times. Nanticoke Creek is designated as a Coldwater Fishery and a Migratory Fishery. However, it is relatively lacking in aquatic life.