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Home > Explore! > Bedrock Geology > Field Localities > Geology at Mt. Pisgah > Figure 2



Figure 2. Glacial grooves (coming toward the viewer) in this exposure at the base of the fire tower attest to the erosive strength of glacial ice. The grooves are developed on thinly bedded schist, with layering that extends from lower left to upper right.


Last updated on April 9, 2009