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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]
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]
Perlite boulders with fireweed in foreground. Perlite softens when it reaches temperatures of 850–900 °C (1,560–1,650 °F). Water trapped in the structure of the material vaporises and escapes, and this causes the expansion of the material to 7–16 times its original volume.
Obsidian (/ ə b ˈ s ɪ d i. ən, ɒ b-/ əb-SID-ee-ən ob-) [5] is a naturally occurring volcanic glass formed when lava extruded from a volcano cools rapidly with minimal crystal growth. It is an igneous rock . [ 6 ]
Glen Ferris Inn, also known as Stockton's Inn, Stockton's Tavern, and Hawkins's Hotel, is a historic hotel located on the bank of the Kanawha River overlooking Kanawha Falls at Glen Ferris, Fayette County, West Virginia. It may have been built as early as 1815. It is a T-shaped brick building in two sections.
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 .
Pages in category "Hotel buildings on the National Register of Historic Places in West Virginia" The following 27 pages are in this category, out of 27 total. This list may not reflect recent changes .
File:Shoshonite lava flows on South Table Mountain, Colorado. Shoshonite is a type of igneous rock.More specifically, it is a potassium-rich variety of basaltic trachyandesite, [1] composed of olivine, augite and plagioclase phenocrysts in a groundmass with calcic plagioclase and sanidine and some dark-colored volcanic glass.