Collection 01 is online · Six natural-history studies

Kudzu Country Club
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Maine

Schoodic Peninsula

The only piece of Acadia National Park on the mainland - all the granite-and-surf drama of Mount Desert Island, with almost none of the crowd.

Schoodic Peninsula

Acadia is one of the most visited parks in the country, and in summer Mount Desert Island shows it - full lots, shuttle lines, traffic on the loop road. Schoodic is the part almost nobody drives the extra forty-five minutes to reach. It's a separate peninsula on the mainland to the east, the only mainland section of the park, and it has the same bones as the famous half: pink granite ledges running straight into the Atlantic, dark spruce behind, and big northern swell breaking white on the rocks.

At Schoodic Point the granite is shot through with black bands - basalt dikes, where molten rock forced its way up through cracks in the older stone and cooled, leaving dark seams you can trace across the pink. The surf hits hard here, exposed straight to open ocean, and on a day with weather offshore the spray comes up over the ledges and the whole point shakes a little. People sit on the rocks for hours watching it. There's a one-way loop road, a few trails up the headlands, and views back across the water to the mountains of the main island.

Schoodic Peninsula - supporting photo

It's the same coast that made Acadia famous - the same rock, the same cold clean water, the same spruce-and-stone Maine - just with room to hear it. Some people come to Acadia for years before they figure out that the best of it might be the part everyone else drives past.

Schoodic Peninsula - supporting photo 2
Schoodic Peninsula - supporting photo 3

Photos - Pink granite ledges at Schoodic Point: Victoria Stauffenberg / National Park Service, Public Domain. Surf at Schoodic Point: John Manard / Flickr, CC BY-SA 2.0. Schoodic Peninsula headland: Giorgio Galeotti / Wikimedia Commons, CC BY-SA 4.0. View back to Mount Desert Island: Fredlyfish4 / Panoramio via Wikimedia Commons, CC BY-SA 4.0. All via Wikimedia Commons.

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