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

Uploaded: 5 May 2020
Last Updated: 19 May 2020

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39.036538, -78.382966 - Facing Northeast Cross bedded oolitic limestone, Cambrian in age and dipping toward the southeast. Oolites are indicators of passive margin sedimentation, formed by rolling back and forth along the floor of warm, shallow seas. Western limb of the Massanutten Synclinorium. The next outcrop to the right (east) is here: https://viewer.gigamacro.com/view/YGvQF7kRonZCqYO8