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The Allegheny River is a 325-mile (523 km) long headwater stream of the Ohio River in western Pennsylvania and New York, United States. The Allegheny River runs from its headwaters just below the middle of Pennsylvania's northern border northwesterly into New York then in a zigzag southwesterly across the border and through Western Pennsylvania to join the Monongahela River at the Forks of the Ohio on the "Point" of Point State Park in Downtown Pittsburgh, Pennsylvania. The Allegheny River is, by volume, the main headstream of both the Ohio and Mississippi Rivers. Historically, the Allegheny was considered to be the upper Ohio River by both Native Americans and European settlers.
The Potomac River is found within the Mid-Atlantic region of the United States and flows from the Potomac Highlands into the Chesapeake Bay. The river is approximately 405 miles (652 km) long, with a drainage area of about 14,700 square miles (38,000 km2). In terms of area, this makes the Potomac River the fourth largest river along the Atlantic coast of the United States and the 21st largest in the United States. Over 5 million people live within the Potomac watershed.
The Mid-Atlantic, comprising the Middle Atlantic states or the Mid-Atlantic states, is a region of the United States generally located between New England and the South Atlantic portion of the Southeastern States. Its exact definition differs upon source, but the region usually includes New York, New Jersey, Pennsylvania, Delaware, Maryland, Washington, D.C., Virginia, and West Virginia. When discussing climate, Connecticut is sometimes included in the region, since its climate is closer to the Middle Atlantic states than the rest of the New England states. The Mid-Atlantic has played an important role in the development of American culture, commerce, trade, and industry.
The Kentucky River is a tributary of the Ohio River, 260 miles (418 km) long, in the U.S. Commonwealth of Kentucky. The river and its tributaries drain much of the central region of the state, with its upper course passing through the coal-mining regions of the Cumberland Mountains, and its lower course passing through the Bluegrass region in the north central part of the state. Its watershed encompasses about 7,000 square miles (18,000 km2). It supplies drinking water to about one-sixth of the population of the Commonwealth of Kentucky.
The Tug Fork is a tributary of the Big Sandy River, 159 miles (256 km) long, in southwestern West Virginia, southwestern Virginia, and eastern Kentucky in the United States. Via the Big Sandy and Ohio rivers, it is part of the watershed of the Mississippi River.
The Levisa Fork is a tributary of the Big Sandy River, approximately 164 miles (264 km) long, in southwestern Virginia and eastern Kentucky in the United States.
The Youghiogheny River, or the Yough for short, is a 134-mile-long (216 km) tributary of the Monongahela River in the U.S. states of West Virginia, Maryland, and Pennsylvania. It drains an area on the west side of the Allegheny Mountains northward into Pennsylvania, providing a small watershed in extreme western Maryland into the tributaries of the Mississippi River. Youghiogheny is a Lenape word meaning "a stream flowing in a contrary direction".
The Shenandoah River is a tributary of the Potomac River, 55.6 miles (89.5 km) long with two forks approximately 100 miles (160 km) long each, in the U.S. states of Virginia and West Virginia. The principal tributary of the Potomac, the river and its tributaries drain the central and lower Shenandoah Valley and the Page Valley in the Appalachians on the west side of the Blue Ridge Mountains, in northwestern Virginia and the Eastern Panhandle of West Virginia.
The Appomattox River is a tributary of the James River, approximately 157 miles (253 km) long, in central and eastern Virginia in the United States, named for the Appomattocs Indian tribe who lived along its lower banks in the 17th century. It drains a cotton and tobacco-growing region of the Piedmont and coastal plain southwest of Richmond.
The York River is a navigable estuary, approximately 34 miles (55 km) long, in eastern Virginia in the United States. It ranges in width from 1 mile (1.6 km) at its head to 2.5 miles (4.0 km) near its mouth on the west side of Chesapeake Bay. Its watershed drains an area of the coastal plain of Virginia north and east of Richmond.
The Elk River is a tributary of the Kanawha River, 172 miles (277 km) long, in central West Virginia in the United States. Via the Kanawha and Ohio rivers, it is part of the watershed of the Mississippi River.
The Hughes River is a tributary of the Little Kanawha River in western West Virginia in the United States. Via the Little Kanawha and Ohio Rivers, it is part of the watershed of the Mississippi River. As measured from the confluence of its north and south forks, the Hughes is 18 mi (29 km) long, and drains a rural area of the unglaciated portion of the Allegheny Plateau.
The Greenbrier River Watershed Association is one of the oldest watershed associations in the state of West Virginia, currently on its 15th year of existence. It has supported the creation of other watershed associations throughout the state and maintains a policy of "upstream courtesy" and "downstream courtesy" with its neighbors.
Chestnut Creek is a river in the state of Virginia.
Cub Creek is a river in the United States state of Virginia. It is a tributary of the Roanoke River.
The Little Nottoway River is a 14.31 mi (23.03 km) long tributary to the Nottoway River in the United States state of Virginia. Located in the southeastern part of the state, it is part of the larger Chowan-Albemarle drainage.
The Middle River is a 70.6-mile-long (113.6 km) river in the U.S. state of Virginia. Flowing entirely within Augusta County, the Middle River joins the North River, which in turn meets the South River at Port Republic to form the South Fork Shenandoah River.
Sinking Creek is a river in the United States state of Virginia. Due to the karst topography northwest of Blacksburg, the river disappears underground and then re-emerges from springs as it flows into the New River.
The Glenshaw Formation is a mapped sedimentary bedrock unit in Pennsylvania, Maryland, West Virginia, and Ohio, of Pennsylvanian age. It is the lower of two formations in the Conemaugh Group, the upper being the Casselman Formation. The boundary between these two units is the top of the marine Ames Limestone. The Conemaugh Group overlies the Upper Freeport coal bed of the Allegheny Formation and underlies the Pittsburgh coal seam of the Monongahela Group.
References
- USGS Geographic Names Information Service
- USGS Hydrologic Unit Map - State of Virginia (1974)
- Salmon, Emily J.; Edward D. C. Campbell, Jr., eds. (1994). The Hornbook of Virginia History (4th ed.). Richmond, VA: Virginia Office of Graphic Communications. ISBN 0-88490-177-7.
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