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Contributing Institution
Maine Geological Survey
Document Type
Image
Identifier
67165
Description
Well-preserved glacial striations are rare in the Unity Pond quadrangle due to the fissile local metasedimentary bedrock, but this nice set along the eastern shore of Unity Pond shows that ice flow was to the southeast (left to right in photo).
Project Name: STATEMAP Unity Pond Surficial
Location
Unity
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
STATEMAP; surficial geology; Unity Pond quadrangle