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Geological subjects: slickenlines on a fault plane

The scale card along the base of the photo is marked in centimetres (black) and millimetres (white bands separated by black lines).

 

A sub-vertical fault plane with sharp bends and slight curves along slickenline striation paths/traces (in non-technical terms, scratches in the rock from frictional drag along the fault surface),

indicating a history of slight and temporary change in displacement direction (part of Eocene age extensional faulting in south-central British Columbia). Location: Warren Creek Road, near Greenwood, British Columbia.

 

C. J.R. Devaney

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Uploaded on August 24, 2018
Taken on August 28, 2011