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Ice Mountain was also detailed in Hu Maxwell and Howard Llewellyn Swisher's History of Hampshire County, West Virginia: From Its Earliest Settlement to the Present (1897), O. F. Morton's History of Hampshire County (1910), and Homer Floyd Fansler's "Ice Mountain: Nature's Deep Freeze" in the July 1959 issue of West Virginia Conservation. [6]
Glaciation in this area of the plateau removed the sharp relief that is seen in the plateau's unglaciated areas. The line of the distant peaks approximates the level of a peneplain that was uplifted to form the plateau. Aerial view of Allegheny Plateau terrain surrounding Weston, West Virginia
Geologic Map of West Virginia. West Virginia's geologic history stretches back into the Precambrian, and includes several periods of mountain building and erosion. At times, much of what is now West Virginia was covered by swamps, marshlands, and shallow seas, accounting for the wide variety of sedimentary rocks found in the state, as well as its wealth of coal and natural gas deposits.
West Virginia was never the site of glacial activity during the Ice Age, but the state was home to creatures like mammoths, mastodons, and giant ground sloths. One local ground sloth, Megalonyx jeffersonii , was subject to the scholarly investigations of Thomas Jefferson , who misinterpreted the large-clawed remains as belonging to a lion-like ...
The rapid retreat of the Cordilleran ice sheet is a focus of study by glaciologists seeking to understand the difference in patterns of melting in marine-terminating glaciers, glaciers whose margin extends into open water without seafloor contact, and land-terminating glaciers, with a land or seafloor margin, as scientists believe the western ...
West Virginia’s youth are required by law to receive vaccines for chickenpox, hepatitis-b, measles, meningitis, mumps, diphtheria, polio, rubella, tetanus and whooping cough – but not Covid-19 ...
West Virginia is situated in the Appalachian Mountains of the Upper South region of the 48 contiguous states. Usually considered part of the South Eastern United States, West Virginia is bounded on the northeast by Pennsylvania and Maryland, on the southeast by Virginia, on the northwest by Ohio, and on the southwest by Kentucky.
The floor of the Teays Valley in West Virginia is 200 feet (61 m) above the entrenched Kanawha and Ohio valley floors, and its bedrock floor is at least 15 feet (4.6 m) above them. The ‘deep stage’ apparently was cut mainly after the diversion of the upper Kanawha (Teays) drainage to the Ohio River (Stout, Ver Steeg, and Lamb, 1943, pp. 78 ...