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The origin of both lakes is unclear. Due to unconsolidated sediments, Lake Drummond should have eroded very quickly. Some geologists have proposed that it may have formed from a meteorite impact. Mountain Lake appears to be a natural dam, formed by the Clinch sandstone, which impounded a mountain stream. The state has nine major river basins. [9]
The wilderness lies north of and in close proximity to Blacksburg, Virginia. It extends for about 8 miles along the northwest slope of Brush Mountain, bounded to the east by a power line, to the northwest by Craig Creek and private property, and to the southeast by Forest road 188.1 along the crest of the mountain. [1] There are no trails in ...
The Mount Rogers area contains a unique record of the geohistory of Virginia. There is evidence from the rocks that volcanoes were part of the landscape. Roughly 760 million years ago, rift-related (divergent) volcanoes erupted along the axis of what later became the Appalachians, and one remnant of that volcanic zone, with its volcanic rocks, still can be seen at Mount Rogers.
During the Triassic, central Virginia was a rift basin. [1] Brachiopods were still present in Virginia during the Mesozoic. [4] On land, the early Mesozoic plants of Virginia included Equisetales, gymnosperms, Cycadeles, cycads, and conifers. This flora is almost identical to that from contemporary deposits in North Carolina. [4]
Boundary of the Cove Mountain wildland in the Jefferson National Forest as identified by the Wilderness Society. [1]The area is located in the Appalachian Mountains of Southwestern Virginia about 4 miles east of Buchanan, Virginia, between the James River on the north, Va 43 on the west, the Blue Ridge Parkway on the south and McFalls Creek Rd (Va 618) on the east.
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
Southern Appalachian low-elevation pine forests occur on a variety of topographic and landscape positions, including ridgetops, upper- and mid-slopes, and in lower elevations (generally below 2,300 feet (700 m)) such as mountain valleys. These forests are dominated by shortleaf pine (Pinus echinata) and Virginia pine (Pinus virginiana).
The area is located in the Appalachian Mountains of Southwestern Virginia, about 11 miles northeast of New Castle, Virginia. It is bounded by Forest road 184 on the north and west, and VA 606 on the south. [2] [3] Trails into the area include: [4] [3] Price Mountain Trail, 10.6 miles; Sulphur Ridge Trail, Forest Trail 149, 2.8 miles; Kelly ...
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