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  2. Cabins, West Virginia - Wikipedia

    en.wikipedia.org/wiki/Cabins,_West_Virginia

    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 .

  3. Mineralwells, West Virginia - Wikipedia

    en.wikipedia.org/wiki/Mineralwells,_West_Virginia

    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]

  4. Middle Mountain Cabins - Wikipedia

    en.wikipedia.org/wiki/Middle_Mountain_Cabins

    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.

  5. National Register of Historic Places listings in West Virginia

    en.wikipedia.org/wiki/National_Register_of...

    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.

  6. Rohrbaugh Cabin - Wikipedia

    en.wikipedia.org/wiki/Rohrbaugh_Cabin

    Rohrbaugh Cabin — also known as Allegheny Cabin — is a historic log cabin located on the eastern slope of North Fork Mountain near Petersburg, Grant County, West Virginia, USA. Rohrbaugh Cabin was built about 1880, and is a 2 + 1 ⁄ 2 -story, "double pen" plan log house built of tulip poplar logs.

  7. Volcanic glass - Wikipedia

    en.wikipedia.org/wiki/Volcanic_glass

    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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