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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.
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 .
There are listings in every one of West Virginia's 55 counties. Listings range from prehistoric sites such as Grave Creek Mound , to Cool Spring Farm in the state's eastern panhandle, one of the state's first homesteads, to relatively newer, yet still historical, residences and commercial districts.
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]
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 .
Blennerhassett Hotel is a historic hotel located at Parkersburg, Wood County, West Virginia. It opened in 1889 and is in the Queen Anne style. [2] The hotel was listed on the National Register of Historic Places in 1982. [1] A full restoration took place in 1986. [3] (The hotel website states that the property is "registered as a national ...
Daniel Boone Hotel is a historic hotel located at Charleston, West Virginia. It is a Classical Revival Style ten story structure with blond brick exterior and tan, modular, stone-looking terra cotta. The building was originally constructed in 1927–1929, expanded in 1936 and again in 1949 to provide a total of 465 rooms, a large ballroom and 3 ...
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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