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7 May 2014

Bedding / cleavage relationships in the Edinburg Formation

Here’s a little scene along Route 340 / 522, north of Front Royal and south of Double Tollgate, Virginia, in the Shenandoah Valley: The rock here is limestone and shale of the Edinburg Formation, a late Ordovician unit that records the transition from passive margin sedimentation to the increasingly ‘dirty’ clastic influence of the Taconian Orogeny. Have a look: I hope you’ll notice there are layers of two distinct lithologies …


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