Dillons Run is a 12.9-mile-long (20.8 km) tributary stream of the Cacapon River, belonging to the Potomac River and Chesapeake Bay watersheds. The stream is located in Hampshire County in the U.S. state of West Virginia's Eastern Panhandle.
Edwards Run is a 7.9-mile-long (12.7 km) tributary stream of the Cacapon River, belonging to the Potomac River and Chesapeake Bay watersheds. The stream is located in Hampshire County in the U.S. state of West Virginia's Eastern Panhandle. Edwards Run is named for Joseph Edwards and his family, whose plantation encompassed most of the stream's course. George Washington surveyed his property in the late 1740s. It is a major source of various species of elodea.
Cherry Run is a 7.2-mile-long (11.6 km) meandering stream that forms the northern section of the boundary between Morgan and Berkeley counties in West Virginia's Eastern Panhandle. While it is mostly non-navigable, Cherry Run provides many pools of varying depths for fishing and swimming. As a tributary of the Potomac River, Cherry Run is part of the Potomac and Chesapeake Bay watersheds.
Limestone Run is a 4.6-mile-long (7.4 km) stream that lies to the east of New Creek Mountain in Mineral County, West Virginia. It is a tributary of the North Branch Potomac River.
Green Spring Run is an 8.9-mile-long (14.3 km) tributary stream of the North Branch Potomac River in Hampshire County in the U.S. state of West Virginia. Green Spring Run rises in Greenwood Hollow north of Springfield and meanders northeast through Green Spring Valley. The South Branch Valley Railroad and Green Spring Road run parallel to the stream. It runs through the community of Green Spring, from which the stream takes its name. From Green Spring, Green Spring Run flows east where it reaches its confluence with the North Branch Potomac shortly before the North Branch joins with the South Branch Potomac River to form the Potomac River.
Big Run is a 4.4-mile-long (7.1 km) tributary stream of the South Branch Potomac River, belonging to the Potomac River and Chesapeake Bay watersheds. Big Run flows through the city of Romney and the campus of the West Virginia Schools for the Deaf and Blind in Hampshire County, West Virginia. The stream is known by local residents as Town Run and Town Creek.
The Frankstown Branch Juniata River is a 46.0-mile-long (74.0 km) tributary of the Juniata River in Blair and Huntingdon Counties, Pennsylvania, in the United States.
Trout Run is an 18.5-mile-long (29.8 km) tributary of the Cacapon River, belonging to the Potomac River and Chesapeake Bay watersheds. The stream is located in Hardy County in West Virginia's Eastern Panhandle. Trout Run rises between Devils Hole Mountain and Great North Mountain near the Virginia state line in the George Washington National Forest. The stream empties into the Cacapon River at Wardensville.
Warm Spring Run is an 11.9-mile-long (19.2 km) non-navigable tributary stream of the Potomac River in Morgan County of West Virginia's Eastern Panhandle. It rises on the eastern side of Warm Springs Ridge and parallels U.S. Route 522 for most of its course. Warm Spring Run enters the Potomac River at Hancock. Warm Spring Run is primarily fed by springs on Warm Springs Ridge, the most well-known of these being the springs at Berkeley Springs State Park in Berkeley Springs through which it flows.
Isaacs Creek is a 15.0-mile-long (24.1 km) tributary stream of Back Creek in Frederick County, Virginia. Isaacs Creek rises on Timber Ridge at the boundary line with Hampshire County, West Virginia, and flows into Back Creek at Grave Hill shortly before Back Creek's confluence with Hogue Creek. The stream is dammed to create Lake Holiday.
Dans Run is a 2.3-mile-long (3.7 km) non-navigable tributary stream of the North Branch Potomac River in Mineral County, West Virginia. Dans Run rises to the east of Patterson Creek Mountain and empties into the North Branch at the community of Dans Run on the old Baltimore & Ohio Railroad. Dans Run Island in the North Branch Potomac, at its confluence with Dans Run, is also named for the small stream.
Town Hill is a mountain range located in Allegany County, Maryland and Bedford and Fulton Counties in Pennsylvania. Its southern end is 2.25 miles northwest of Kiefer in Allegany County. It trends northeasterly, and ends about 1.5 miles south of the town of Emmaville in Fulton County. Its highest elevation is 2000 feet.
Paw Paw Creek is a 14.4-mile-long (23.2 km) tributary of the Monongahela River in West Virginia.
The Devonian Old Port Formation is a mapped bedrock unit in Pennsylvania, USA. Details of the type section and of stratigraphic nomenclature for this unit as used by the U.S. Geological Survey are available on-line at the National Geologic Map Database. Current nomenclature usage by U.S. Geological Survey restricts the name Old Port Formation to Pennsylvania, but correlative units are present in adjacent states.
Wheatfield is an unincorporated community in Shenandoah County, in the U.S. state of Virginia.
Grove Hill is an unincorporated community in Page County, in the U.S. state of Virginia.
Mill Run is a 9.1-mile-long (14.6 km) tributary stream of the South Branch Potomac River, belonging to the Potomac River and Chesapeake Bay watersheds. The stream is located in Hampshire County in the Eastern Panhandle of the U.S. state of West Virginia. Mill Run rises on Nathaniel Mountain and flows northeast, then northwest into the South Branch south of Romney near Hampshire Park on South Branch River Road.
The Waynesboro Formation is a limestone, dolomite, and sandstone geologic formation in Virginia, Maryland, Pennsylvania and West Virginia. It some areas it is composed of limestone and dolomite. The Waynsboro Formation is one of the formations that make up the Shenandoah Valley. It dates back to the Cambrian period and is not considered fossiliferous.
Warren Point is a former town in the southwest corner of Warren Township, Franklin County, Pennsylvania. It was located on the north side of Licking Creek, and at the southwest end of Keefer Mountain, and approximately two miles west of Yeakle Mill.
