By: magic-gigapans
Image: Callan Bentley, Mid-Atlantic Geo-Image Collection
License: Creative Commons Non Commercial ⧉

Uploaded: 1 May 2020
Last Updated: 19 May 2020

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This is the eastern limb of the Blue Ridge Anticlinorium, where Cambrian-aged quartzites of the Weverton Formation dip moderately east. Bedding (visible as dark bands of heavy minerals) is cut across by steeply-dipping quartz veins and at least two joint sets, stained by iron oxides.