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The clay found in the cliffs on the north shore of Long Island, particularly in areas like the North Shore’s bluffs and cliffs, primarily comes from glacial deposits left behind during the last Ice Age. This region was heavily influenced by glacial activity, particularly by the Wisconsin Glaciation, which occurred about 21,000 years ago. As the glaciers advanced and then retreated, they scraped and eroded the land, carrying and depositing a mix of sediments, including clay, silt, sand, and gravel.
When the glaciers melted, they left behind these sediments, creating the layers of clay found in the cliffs. This process is part of what shaped the unique geology of Long Island, contributing to its varied landscape, including the prominent cliffs on the north shore.