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The largest salt deposit under the Great Lakes formed during the late Silurian to early Devonian periods, around 400 million years ago, when the region was covered by a shallow sea. As the climate changed and the sea evaporated, it left behind concentrated saline water, which eventually precipitated and settled as thick layers of salt. Geological processes, including tectonic shifts, further compressed and buried these deposits over millions of years, leading to the vast salt formations we see today beneath the Great Lakes.

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