The West Branch Schuylkill River (also known simply as the West Branch) is an approximately

tributary A tributary, or affluent, is a stream or river that flows into a larger stream or main stem (or parent) 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 ...

of the

Schuylkill River The Schuylkill River ( , ) is a river running northwest to southeast in eastern Pennsylvania. The river was improved by navigations into the Schuylkill Canal, and several of its tributaries drain major parts of Pennsylvania's Coal Region. It fl ...

in central

Schuylkill County, Pennsylvania Schuylkill County (, ; Pennsylvania Dutch: Schulkill Kaundi) is a county in the Commonwealth of Pennsylvania. It is located in the heart of Pennsylvania's Coal Region and is part of Northeastern Pennsylvania. As of the 2020 census, the popula ...

, USA, with a watershed approximately in size. Several small communities are located in the watershed, which include Beaver Meadows, Buck Run, Glen Dower, Minersville, Pottsville, Cressona, and Schuylkill Haven. Mild amounts of

acid mine drainage Acid mine drainage, acid and metalliferous drainage (AMD), or acid rock drainage (ARD) is the outflow of acidic water from metal mines or coal mines. Acid rock drainage occurs naturally within some environments as part of the rock weathering ...

affect the West Branch and its tributaries. From its headwaters near

Interstate 81 Interstate 81 (I-81) is a north–south (physically northeast–southwest) Interstate Highway in the eastern part of the United States. Its southern terminus is at I-40 in Dandridge, Tennessee; its northern terminus is on Wellesley Island ...

, the river flows southeast through several

water gap A water gap is a gap that flowing water has carved through a mountain range or mountain ridge and that still carries water today. Such gaps that no longer carry water currents are called wind gaps. Water gaps and wind gaps often offer a prac ...

s in the

Ridge-and-Valley Appalachians The Ridge-and-Valley Appalachians, also called the Ridge and Valley Province or the Valley and Ridge Appalachians, are a physiographic province of the larger Appalachian division and are also a belt within the Appalachian Mountains extending ...

, ending at its confluence with the Schuylkill River in Schuylkill Haven.

Course

The West Branch's source is several small ponds east of

, near the small community of Buck Run. The river flows east-northeast, paralleling Valley Road and later the Heckscherville Road. Near Heckscherville, it receives small tributaries Dyer Run, Wagner Run, and Wheeler Creek, all on the

left bank In geography, a bank is the land alongside a body of water. Different structures are referred to as ''banks'' in different fields of geography, as follows. In limnology (the study of inland waters), a stream bank or river bank is the terrai ...

. It then flows south and southeast past Minersville, and finally east through a narrow canyon, where it receives Indian Run on the

right bank In geography, a bank is the land alongside a body of water. Different structures are referred to as ''banks'' in different fields of geography, as follows. In limnology (the study of inland waters), a stream bank or river bank is the terrai ...

. After exiting the canyon, it turns south and enters an increasingly wide valley. At Cressona, it receives Panther Creek on the right bank and Beaver Creek on the left bank. As the river enters Schuylkill Haven it merges with the Schuylkill River on the right bank.https://maps.google.com

References

{{authority control Rivers of Schuylkill County, Pennsylvania Rivers of Pennsylvania Tributaries of the Schuylkill River

Course

See also

References