Preview
Contributing Institution
Maine Geological Survey
Document Type
Image
Identifier
67281
Description
Well-preserved glacial striations are rare in the Unity quadrangle due to the fissile local metasedimentary bedrock, but this nice set along Sandy Stream shows that ice flow was to the southeast (same orientation as marker, right to left in photo).
Project Name: STATEMAP Unity 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; Unity quadrangle; surficial geology; striations