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Harveys Creek

Rivers of Luzerne County, PennsylvaniaRivers of PennsylvaniaTributaries of the Susquehanna River
Harveys Creek looking upstream 1
Harveys Creek looking upstream 1

Harveys Creek (also known as Harvey Creek or Harvey's Creek) is a tributary of the Susquehanna River in Luzerne County, Pennsylvania, in the United States. It is approximately 14.5 miles (23.3 km) long and flows through Harveys Lake, Lake Township, Lehman Township, Jackson Township, and Plymouth Township. The creek's watershed has an area of 46.3 square miles (120 km2). The creek has four named tributaries, which are known as Bear Hollow Creek, Paint Spring Run, Pikes Creek, and East Fork Harveys Creek. The watershed is designated as a High-Quality Coldwater Fishery and a Migratory Fishery above Pikes Creek and as a Coldwater Fishery and a Migratory Fishery below it. The creek's source is Harveys Lake, the largest natural lake in Pennsylvania. Harveys Creek was used as a water supply as early as the beginning of the 1900s. A number of bridges have been constructed over the creek since the 1920s, and it has been dammed by the Bryant Pond Dam. It is possible to canoe on part of the creek. Rock formations consisting of sandstone and shale occur in the watershed.

Excerpt from the Wikipedia article Harveys Creek (License: CC BY-SA 3.0, Authors, Images).

Harveys Creek
Canal Street, Plymouth Township

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Wikipedia: Harveys CreekContinue reading on Wikipedia

Geographical coordinates (GPS)

Latitude Longitude
N 41.2197 ° E -76.0165 °
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Address

Canal Street

Canal Street
18634 Plymouth Township
Pennsylvania, United States
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Harveys Creek looking upstream 1
Harveys Creek looking upstream 1
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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.