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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.
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West Virginia joined Kentucky and Utah, which also recognize coal as a state mineral or rock. The drive to name coal as an official state symbol was initiated by a high school student from Wharncliffe, West Virginia, who initiated her project at a school fair and collected 2,500 signatures on a petition that was submitted to legislators. [85]
This list of the Paleozoic life of West Virginia contains the various prehistoric life-forms whose fossilized remains have been reported from within the US state of West Virginia and are between 538.8 and 252.17 million years of age.
This list of the prehistoric life of West Virginia contains the various prehistoric life-forms whose fossilized remains have been reported from within the US state of ...
Largest cave in West Virginia. Shavers Mountain Spruce-Hemlock Stand: 1974 Randolph: Federal An old-growth stand of red spruce and hemlock trees. Part of Monongahela National Forest. Sinnett-Thorn Mountain Cave System: 1973 Pendleton: Private Cave system with waterfalls and deep pits.
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.
A geode (/ ˈ dʒ iː. oʊ d /; from Ancient Greek γεώδης (geṓdēs) 'earthlike') is a geological secondary formation within sedimentary and volcanic rocks. Geodes are hollow, vaguely spherical rocks, in which masses of mineral matter (which may include crystals) are secluded.