Ripple marks and trace fossils in the Rose Hill Formation

Good morning!

Here are some ripple marked strata in the Silurian-aged Rose Hill Formation from West Virginia:

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Tilting of these strata occurred long after the Silurian – during the late Paleozoic Alleghanian Orogeny — an application of the principle of relative dating known as “Original Horizontality.”

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There are also trace fossils to be seen on these bedding planes.

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This was another site that I was introduced to in April, on the GMU sedimentology and stratigraphy field trip led by Rick Diecchio.

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