Abstract or Description
This map shows the bedrock geology of the Belgrade Lakes area. The meta-sedimentary rocks are dominantly silurian in age, while intrusive rocks are devonian-aged. Silurian rocks begin with an 'S' in their labels; devonian rocks with a 'D'. Lakes are overlayed as transparent blue polygons. Thin brown contour lines indicate topographic relief at 50-foot intervals.
Source Data Note
The data was collected from Maine Office of GIS.
Recommended CitationFereday, Wyatt "Belgrade Lakes Region: Bedrock Geology," Atlas of Maine: Vol. 2010: No. 1, Article 11.
Available at: https://digitalcommons.colby.edu/atlas_docs/vol2010/iss1/11