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Exposed on the northern bank of the Chesapeake and Ohio Canal near the downstream end of "Widewater" (upstream of the Old Anglers Inn access point), these rocks are the result of ancient mountain-building processes. These rocks, the Mather Gorge Formation, were originally deposited as layers of sand and mud i...
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Exposed on the northern bank of the Chesapeake and Ohio Canal near the downstream end of "Widewater" (upstream of the Old Anglers Inn access point), this antiform is the result of ancient mountain-building processes. A fold that goes up in the middle is called an "antiform," and if there is stratigr...
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This Antiform is located in the southern region of Fort Valley, Virginia. This fold is in shale from the Devonian Needmore formation. This exposed fold is a parasitic fold on the larger Massanutten Synclinorium regional structure. View of the Camera is rougly south For more context see these two other GigaPans also ...
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