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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.
West Virginia is the 10th-smallest state by area and ranks as the 12th-least populous state, with a population of 1,793,716 residents. [5] The capital and most populous city is Charleston with a population of 49,055. West Virginia was admitted to the Union on June 20, 1863, and was a key border state during the American Civil War.
At the close of Mississippian time, about 310 million years ago, West Virginia was essentially a land area, subject to erosion. Early in the succeeding Pennsylvanian Period, the area dropped to near sea level and for more than 50 million years continued to sink at about the same rate that deposition was taking place.
Canyons and gorges of West Virginia (9 P) Caves of West Virginia (10 P) Chesapeake Bay watershed (9 C, 60 P) Cliffs of West Virginia (2 P) I. Islands of West Virginia ...
Former West Virginia Governor William A. MacCorkle described him as a man who knew the land "as a farmer knows a field." Beginning in 1898, Page teamed with northern and European-based investors to take advantage of the undeveloped area.
This is a list of the National Natural Landmarks (NNLs) in West Virginia.There are sixteen in all — five are wetlands (such as bogs and swamps), three are forests, six are limestone caves/karst, and two are rock formations.
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