By: rkohrs
Image: Callan Bentley
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License:
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Uploaded: 31 Dec 2019
Last Updated: 31 Dec 2019
1.02 gigapixels
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Outcrop of the late-Ordovician-aged Martinsburg Formation (turbidites/flysch) shed off the Taconian Orogen to the east into the adjacent deep marine basin. The strata were later tilted and cleaved during Alleghanian mountain-building.