By: rkohrs
Image: Russ Kohrs ⧉
License: Creative Commons Share Alike ⧉

Uploaded: 16 Apr 2020
Last Updated: 16 Apr 2020

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Juniata Formation redbeds and point bar deposits. Interbedded fluvial units. Note the abrubt change in lithology center screen, where massive red micaceous scandstones give way to interbedded floodplain and channel deposits. Most likely, this is a crevasse splay deposit where repeated outflows from a gap in an ancient stream levee were deposited. You can read more about this deposite here: https://blogs.agu.org/mountainbeltway/2010/03/25/transect-debrief-5-sedimentation-continues/