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The average salary for a water resource specialist is $157,740 per year. And the Bureau of Labor Statistics (BLS) estimates 8% job growth, which is much higher than average. This means that you ...
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]
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
Southwest Virginia, often abbreviated as SWVA, is a mountainous region of Virginia in the westernmost part of the commonwealth.Located within the broader region of western Virginia, Southwest Virginia has been defined alternatively as all Virginia counties on the Appalachian Plateau, all Virginia counties west of the Eastern Continental Divide, or at its greatest expanse, as far east as ...
The Cumberland Plateau (also called the Appalachian Plateau) and the Cumberland Mountains are in the south-west corner of Virginia, below the Allegheny Plateau. In this region rivers flow northwest, with a dendritic drainage system, into the Ohio River basin. [14] This region corresponds to the EPA's Central Appalachians (#69) region.
Beginning at the junction of the Cowpasture and Jackson rivers in the Allegheny Mountains of western Virginia, the James River flows for about 340 miles (550 km) to Chesapeake Bay, where it has become 5 miles (8 km) wide. The course of the river was formed over hundreds of millions of years as it followed faults in the earth's crust.
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.
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 ...
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