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Pages in category "Mountain ranges of Virginia" The following 12 pages are in this category, out of 12 total. This list may not reflect recent changes. A.
Little Cobbler Mountain (North Cobbler Mountain) – Elevation 1,447 ft (441 m) Big Cobbler Mountain (South Cobbler Mountain) – Elevation 1,562 ft (476 m) 38°50′19″N 77°57′10″W / 38.8387°N 77.9528°W / 38.8387; -77.9528 ( Big Cobbler Mountain (South Cobbler Mountain
Hoop Petticoat Gap, elevation 860 feet, on U.S. Route 50 in Virginia to Romney; Paddy Gap in Paddy Mountain, elevation 1,400 feet, Brocks Gap in Little North Mountain, elevation 1,020 feet, on Virginia State Route 259 to North Mountain; Dry River Gap on U.S. Route 33 in Virginia to Harrisonburg-Franklin; Buffalo Gap on Virginia State Route 42 ...
The Hamilton Group is a Devonian-age geological group which is located in the Appalachian region of the United States.It is present in New York, Pennsylvania, Maryland, Ohio, West Virginia, northwestern Virginia and Ontario, Canada, [1] [2] and is mainly composed of marine shale with some sandstone.
Mount Rogers in the Blue Ridge Mountains is the highest peak in the U.S. Commonwealth of Virginia. This article comprises three sortable tables of the major mountain peaks of Virginia . This article defines a significant summit as a summit with at least 100 meters (328.1 feet) of topographic prominence , and a major summit as a summit with at ...
The Virginia Piedmont is largely characterized by rolling hills and numerous ridges near the boundary with the Blue Ridge Mountains. Lying between the mountain and coastal plain regions, the Piedmont region is a naturally diverse landscape. [2] The bedrock consists mostly of gneiss, schist, and granite rocks at a typical depth of between 2 and ...
The climate of Virginia varies according to location, and becomes increasingly warmer and humid farther south and east. [19] Most of the state has a humid subtropical climate, from the Blue Ridge Mountains and southern Shenandoah Valley to the Atlantic coast. In the Blue Ridge Mountains, the climate becomes subtropical highland. [citation needed]
Rockfish Gap is underlain by greenstones of the Catoctin Formation, a late Neoproterozoic geologic unit exposed throughout the Blue Ridge Mountains in Virginia, Maryland, and southern Pennsylvania. Catoctin greenstones were originally erupted as basaltic lava flows 550 to 565 million years ago and later metamorphosed and deformed during the ...