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Geomorphology Of The Allegheny Mountains Of East Central West Virginia. Open Access Deposited
The Allegheny Mountains of east-central West Virginia were imperfectly peneplained in pre-Schooley time. There is no evidence that any external base level has affected this region since uplift of the pre-Schooley surface, i.e., no peneplains controlled by a base level outside the area have developed since pre-Schooley time. The region has been lowered by differential mass-wasting ever since this uplift.
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