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- Most glacial activity in Maine involved large continental ice sheets, but the erosional effects of alpine glaciers are clearly evident in two of the highest groups of mountains: Mt. Katahdin and neighboring peaks in Baxter State Park, and Sugarloaf Mountain and other nearby peaks in western Maine.
www.maine.gov/dacf/mgs/explore/surficial/facts/surficial.htm
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Oct 6, 2005 · Most glacial activity in Maine involved large continental ice sheets, but the erosional effects of alpine glaciers are clearly evident in two of the highest groups of mountains: Mt. Katahdin and neighboring peaks in Baxter State Park, and Sugarloaf Mountain and other nearby peaks in western Maine.
The Ice Age had a profound effect on the Maine landscape. This effect is very pronounced in the Down East region, where a vast sheet of glacial ice sculpted Cadillac and surrounding mountains, carved out the Sommes Sound fjord, and left spectacular sand barrens.
- Field Localities
- Fact Sheets
- Geologic Maps and Digital Data
- Related Reading
- Soils
Originally published on the web as the Survey's "Site of the Month," these sites include more detailed descriptions of geologic features, field trips, and localities.
Available surficial geologic mapsStatewide geologic mapsMaine Secretary of State Kids' Page - State Soil - ChesuncookNatural Resources Conservation Servicemelting glacier. Sediment samples and other data reveal that Maine’s climate at the time probably resembled far north-ern Canada or portions of Greenland that are today within the Arctic Cir-cle. Glaciers shaped the state of Maine, covering every inch of its land and weighing down the surface so much so that when the ice rapidly
Jan 20, 2011 · Glaciers range from small alpine glaciers (which are mostly confined to valleys) to giant continental ice sheets such as those found today in Antarctica and Greenland. Q4. How many times was Maine covered by glacial ice during the Ice Age?
In Maine, the great majority of moraines occur in the southern part of the state, where lingering crustal depression from the weight of the ice sheet caused the ocean to flood the coastal lowland as the ice withdrew. Marine waters lapped against the glacier margin and icebergs calved into the sea.
Most glacial activity in Maine involved the large continental ice sheets, but the erosional effects of alpine glaciers are clearly evident in two of the highest groups of mountains: Mt. Katahdin and neighboring peaks in Baxter State Park, and Sugarloaf Mountain and other nearby peaks in western Maine. Local glaciers eroded deep semi-circular ...