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Contributing Institution
Maine Geological Survey
Document Type
Image
Identifier
9683
Description
Photo 8. Fine-grained mylonitic gneiss of the Ray Corner Mylonite Suite (rcm) cut by light gray veins of pseudotachylyte. Sudden, brittle failure at depth in the earth can generate intense frictional heating which causes melting along the fault surface. The melt then invades any open fractures and solidifies instantly, producing a rock similar to volcanic glass, called pseudotachylyte. This is an indicator of ancient faulting that probably produced earthquakes. Pavement outcrop approximately 700 meters west-northwest (N80W) of Ray Corner, Knox.
Project Name: Bedrock Geology Brooks West
Exact Creation Date
6-8-2012
Location
Knox
Supplemental Rights
Credit must be given to the photographer and the Maine Geological Survey when this photo is displayed, reproduced, distributed and/or used in derivative works.
Keywords
bedrock mapping; outcrop; STATEMAP