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Cabins is an unincorporated community on the North Fork South Branch Potomac River in Grant County, West Virginia, United States. [2] Cabins lies within the Spruce Knob–Seneca Rocks National Recreation Area of the Monongahela National Forest .
Middle Mountain Cabins are a set of three historic cabins located in the Monongahela National Forest near Wymer, Randolph County, West Virginia. They were built in 1931, and consist of the Main Cabin and Cabins 1 and 2. The Main Cabin is a one-story, rectangular, stained log building measuring approximately 22 feet by 20 feet.
Metro Valley 21 Lewis: 13 Mountain Lakes 22 Lincoln: 2 Metro Valley 23 Logan: 5 Metro Valley 24 Marion: 24 Mountaineer Country 25 Marshall: 12 Northern Panhandle 26 Mason: 12 Metro Valley 27 McDowell: 17 New River/Greenbrier Valley 28 Mercer: 20 New River/Greenbrier Valley 29 Mineral: 11 Potomac Highlands 30 Mingo: 8 Metro Valley 31 Monongalia ...
Mineralwells, also known as Mineral Wells, is a census-designated place (CDP) in Wood County, West Virginia, United States. It is part of the Parkersburg-Marietta-Vienna, WV-OH Metropolitan Statistical Area. The population was 1,950 at the 2010 census. [3] The population was 2216 at the 2021 census. [5]
Germany Valley is a scenic upland valley high in the Allegheny Mountains of eastern West Virginia originally settled by German (including Pennsylvania Dutch) farmers in the mid-18th century. It is today a part of the Spruce Knob–Seneca Rocks National Recreation Area of the Monongahela National Forest , although much ownership of the valley ...
Yellowstone National Park is symbolic of the American West to many. It became the world’s first national park when President Ulysses Grant signed it into existence in 1872. Most Yellowstone ...
Wells Inn, also known as the Hotel Wells, is a historic hotel located at Sistersville, Tyler County, West Virginia, United States. It was built in 1894–1895, and is a two-story, brick building featuring a two-story verandah .
Magma rich in silica and poor in dissolved water is most easily cooled rapidly enough to form volcanic glass. As a result, rhyolite magmas, which are high in silica, can produce tephra composed entirely of volcanic glass and may also form glassy lava flows. [2] Ash-flow tuffs typically consist of countless microscopic shards of volcanic glass. [3]
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