The Blue Ridge Parkway is a National Parkway and All-American Road in the United States, noted for its scenic beauty. The parkway, which is America's longest linear park, runs for 469 miles (755 km) through 29 Virginia and North Carolina counties, linking Shenandoah National Park to Great Smoky Mountains National Park. It runs mostly along the spine of the Blue Ridge, a major mountain chain that is part of the Appalachian Mountains. Its southern terminus is at U.S. 441 on the boundary between Great Smoky Mountains National Park and the Cherokee Indian Reservation in North Carolina, from which it travels north to Shenandoah National Park in Virginia. The roadway continues through Shenandoah as Skyline Drive, a similar scenic road which is managed by a different National Park Service unit. Both Skyline Drive and the Virginia portion of the Blue Ridge Parkway are part of Virginia State Route 48, though this designation is not signed.
The Cumberland Mountains are a mountain range in the southeastern section of the Appalachian Mountains. They are located in western Virginia, eastern edges of Kentucky, and eastern middle Tennessee, including the Crab Orchard Mountains. Their highest peak, with an elevation of 4,223 feet (1,287 m) above mean sea level, is High Knob, which is located near Norton, Virginia.
The Allegheny Front is the major southeast- or east-facing escarpment in the Allegheny Mountains in southern Pennsylvania, western Maryland, and eastern West Virginia, USA. The Allegheny Front forms the boundary between the Ridge-and-Valley Appalachians to its east and the Appalachian Plateau to its west. The Front is closely associated with the Appalachian Mountains' Eastern Continental Divide, which in this area divides the waters of the Ohio/Mississippi river system, flowing to the Gulf of Mexico, from rivers flowing into Chesapeake Bay and from there into the Atlantic Ocean.
The Cacapon River, located in the Appalachian Mountains of West Virginia's Eastern Panhandle region, is an 81.0-mile-long (130.4 km) river known for its fishing, boating, wildlife, and scenery. As part of the Potomac River watershed, it is an American Heritage River.
The Trough is a 6-mile long wooded gorge carved by the South Branch Potomac River (SBPR) and situated in the Allegheny Mountains of Hampshire and Hardy Counties, West Virginia, USA. The area was the site of a 1756 skirmish of the French and Indian War, known as the "Battle of the Trough".
Back Creek is a 59.5-mile-long (95.8 km) tributary of the Potomac River that flows north from Frederick County, Virginia, to Berkeley County in West Virginia's Eastern Panhandle. Back Creek originates along Frederick County's border with Hampshire County, West Virginia, at Farmer's Gap in the Great North Mountain. Its name reflects its location to the west of North Mountain. The perspective of colonists from the east in the 18th century led them to call it "Back Creek", because it lay to the back of North Mountain.
Sleepy Creek Mountain is a mountain ridge in the Ridge-and-Valley Appalachians on the border between Morgan and Berkeley counties in the Eastern Panhandle of West Virginia. The long-distance Tuscarora Trail traverses the southern ridge and northern bench of the mountain.
Blue Ridge Mountain, also known as Blue Mountain, is the colloquial name of the westernmost ridge of the Blue Ridge Mountains in northern Virginia and the Eastern Panhandle of West Virginia. The Appalachian Trail traverses the entire length of the mountain along its western slope and crest.
Sir Johns Run is an unincorporated community hamlet at the mouth of Sir Johns Run on the Potomac River in Morgan County, West Virginia northwest of Berkeley Springs. It is bound to its west by the Widmeyer Wildlife Management Area and to its east by Warm Springs Ridge. While Sir Johns Run formerly served on the old Baltimore and Ohio Railroad mainline as an early passenger station for Berkeley Springs, today it is primarily a residential community of Berkeley Springs accessible by Sir Johns Run Road. Sir Johns Run had its own post office in operation from 1850 to 1938. Today, the stream and its namesake hamlet are a site on the Washington Heritage Trail.
North Mountain is a mountain ridge within the Ridge-and-valley Appalachians in the U.S. states of Virginia and West Virginia.
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.
South Mountain is the northern extension of the Blue Ridge Mountain range in Maryland and Pennsylvania. From the Potomac River near Knoxville, Maryland, in the south, to Dillsburg, Pennsylvania, in the north, the 70-mile-long (110 km) range separates the Hagerstown and Cumberland valleys from the Piedmont regions of the two states. The Appalachian National Scenic Trail follows the crest of the mountain through Maryland and a portion of Pennsylvania.
Clinch Mountain is a mountain ridge in the U.S. states of Tennessee and Virginia, lying in the ridge-and-valley section of the Appalachian Mountains. From its southern terminus at Kitts Point, which lies at the intersection of Knox, Union and Grainger counties near Blaine, Tennessee, it runs in a generally east-northeasterly direction to Garden Mountain near Burke's Garden, Virginia. It separates the Clinch River basin, to the north, and the Holston River basin, to the south.
Powell Mountain is a mountain ridge of the Ridge-and-valley Appalachians of the Appalachian Mountains. It is a long and narrow ridge, running northeast to southwest, from about Norton, Virginia to near Tazewell, Tennessee. It separates the Clinch River basin and the Powell River basin of Powell Valley. It was named for an 18th-century explorer.
In the U.S. state of Virginia, U.S. Route 220 (US 220) is a major north-south state highway that extends from the North Carolina state line through Roanoke to the West Virginia state line. South of Roanoke, US 220 is a four-lane highway within the proposed Interstate 73 (I-73) corridor. US 220 narrows to two lanes north of Roanoke, connecting to I-64 near Clifton Forge and then paralleling the Appalachian Mountains north-northeasterly in the direction of Cumberland, Maryland.
State Route 39 is a primary state highway in the U.S. state of Virginia. The state highway runs 59.17 miles (95.22 km) from the West Virginia state line near Mountain Grove, where the highway continues as West Virginia Route 39, east to U.S. Route 11 in East Lexington. SR 39 connects Lexington with several communities formed around hot springs in Bath County. In Rockbridge County, the state highway passes through the town of Goshen and Goshen Pass, a gorge formed by the Maury River.
The Potomac Water Gap is a double water gap in the Blue Ridge Mountains, located at the intersection of the states of Virginia, West Virginia and Maryland, near Harpers Ferry. At 256 feet (78 m), it is the lowest crossing of the Blue Ridge Mountains.
U.S. Route 522 is a part of the U.S. Highway System that runs from Powhatan, Virginia to Selinsgrove, Pennsylvania. In West Virginia, the U.S. highway runs 19.0 miles (30.6 km) from the Virginia state line near Ridge north to the Maryland state line at the Potomac River in Hancock just south of Hancock, Maryland. US 522 passes through Ridge and Valley Province of the Appalachian Mountains in the Eastern Panhandle of West Virginia. The portion of the U.S. highway in West Virginia serves to connect Winchester with Hancock via Berkeley Springs, the county seat of Morgan County. US 522 is part of the National Highway System for its entire length in West Virginia.
The Ridgeley sandstone is a sandstone or quartzite of Devonian age found in the Appalachian Mountains of Pennsylvania, Maryland, West Virginia, and Virginia, United States. The Ridgeley is fine-grained, siliceous, calcareous in its lower strata, sometimes fossiliferous, and sometimes locally pebbly or conglomeritic. Varying in thickness from 12 to 500 feet, this rock slowly erodes into white quartz sand that often washes or blows away, but sometimes accumulates at large outcrops. When freshly broken, the rock is white, but outcrop surfaces are often stained yellowish by iron oxides.
