Creator

Lindsay Spigel

Preview

image 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

 
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