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Glacial erratics on Long Island originate from the Canadian Shield, where rocks were picked up and transported by glaciers during the last Ice Age, approximately 20,000 years ago. As the glaciers advanced and then retreated, they deposited these large boulders across Long Island. The erratics are often composed of various types of rock, differing from the local geology, which provides evidence of their glacial origins. Today, they can be found scattered throughout the landscape, serving as a reminder of the region's glacial history.

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