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The Atlantic Seaboard Fall Line, or Fall Zone, is a 900-mile (1,400 km) escarpment where the Piedmont and Atlantic coastal plain meet in the eastern United States. [2] Much of the Atlantic Seaboard fall line passes through areas where no evidence of faulting is present.
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 ...
A significant portion of the Divide forms part of the border between West Virginia and Virginia along Allegheny Mountain and then Peters Mountain, separating the Greenbrier River and James River watersheds. It then makes a dramatic arc to the east around the Sinking Creek valley, and then follows the hill crest east of Blacksburg, Virginia. [3] [4]
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
During the warm late Eocene, sea levels were high, and the tidewater region of Virginia lay in the coastal shallows. The shore of eastern North America, about where Richmond, Virginia is today, was covered with thick tropical rainforest, and the waters of the gently sloping continental shelf were rich with marine life that was depositing dense layers of lime from their microscopic shells.
Painted relief map of the Tidewater region on the east coast of the United States in darkest green to one shade lighter green to the west. "Tidewater" is a term for the north Atlantic Plain region of the United States. It is located east of the Atlantic Seaboard Fall Line and north of the Deep South.
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]
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 ...