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Museum Hours
Mondays 1:00 - 4:00
Wednesdays 1:00 - 4:00
Fridays 1:00 - 4:00
Saturdays 1:00 - 4:00
Through early October
Admission is Free

Phone
207·789·5445

Lincolnville Timeline


THE PRE-EUROPEAN ERA



Ten thousand years ago a glacial ice sheet covered Lincolnville to a depth of several thousand feet. Look around and see the evidence of the Ice Age everywhere.

1. The hills are "bald" or nearly so, with only a thin skin of topsoil. Climb to the top of Bald Rock or Cameron, Ducktrap, Frohock, Derry or Levensellar Mountains to see how the hills were scraped clean by the ice.
2. Several ponds were formed in glacier-scraped depressions which filled with melting glacial ice: Norton, Coleman Levensellar, Moody and Pitcher Ponds.
3. Rocks, carried along in the slow-moving glacier, were dropped with the ice melted. These rocks were moved by early farmers to boundary walls, still visible all around town. If the land was never farmed the surface may be covered with boulders of all sizes.
4. Gravel beds were deposited by glacial rivers flowing off the melting ice.


Stone, shell, bone and ceramic artifacts found along Lincolnville’s shores show that native peoples hunted and fished here as long as 6,000 years ago. The earliest population may have been the Moorehead Phase or "Red Paint" people, skilled ocean fishermen who hunted swordfish in a much warmer Gulf of Maine.Balanced Rock Several shell middens, or refuse heaps, have eroded out of the banks of our shoreline, marking early native people’s campsites.


European explorers, starting with the Vikings and included John Cabot and Samuel de Champlain and others, probably sailed by Lincolnville’s shore on their visits to the Maine coast, though there is no record that they ever landed here. The earliest dated artifact of European origin found here are some fragments of a clay pipe made between 1650 and 1660, probably for trade with the native population. The pipe could have been brought to Lincolnville from Fort Pentagoet across the Bay in Castine.


Balance Rock on Fernald’s Neck is a striking example of a glacial erratic, or large glacier-borne boulder.

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