Title
Preview
Contributing Institution
Maine Geological Survey
Document Type
Image
Identifier
69768
Description
Photo 8: Alternating layers of light gray feldspathic and micaceous quartz-rich granofels (bottom) and darker gray sillimanite-rich mica schist (top) of the Cape Elizabeth Formation (Oce) of the Casco Bay Group. Prior to metamorphism, these were alternating beds of quartz-rich sand and fine-grained mudstone. Sillimanite (white knots in the upper layer) is an aluminous metamorphic index mineral whose presence indicates these rocks were once heated to over 900°F during metamorphism. Plummer Point, Damariscotta River, South Bristol.
Project Name: STATEMAP Bristol Bedrock24k
Exact Creation Date
7-30-2021
Location
South Bristol
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