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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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Toggle Minimize gigapan_commentRon Schott (February 16, 2012, 02:42PM )
Damn! That's a good one. Well done, Alan!