Wednesday, February 23, 2011

Serpentinite exposure

Click on the image to enlarge.           Photo © Daniel R. Snyder
Serpentinite exposure adjacent to an extensive occurrence of Josephine peridotite.  Because serpentine can't accommodate the iron in the peridotite protolith, much of this is taken up as hematite, visible as  brick-red layers in the exposure. Road cut opposite Eight Dollar Mountain, Josephine County, SW Oregon. Rock hammer for scale is in the white circle at the bottom of the photograph.

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