The Great Lakes exist because glaciers the size of mountains carved massive valleys across North America during the last Ice Age, then melted and filled them with water.
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During the last glacial period, ice sheets over a mile thick scraped the bedrock like a giant file, creating interconnected basins that couldn't drain naturally afterward.
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The glaciers didn't just carve downward—they pushed sediment ahead of them, creating natural dams that trapped meltwater and shaped the lakes' exact boundaries today.
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Lake Superior's basin formed when glaciers exploited a weak zone in ancient bedrock, making it Earth's largest freshwater lake by surface area.
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The lakes' water levels still rise and fall because the land beneath them is slowly rebounding upward after the glacier's immense weight finally lifted.
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Isostatic rebound means the northern lake shores are rising while southern shores sink, gradually tilting the entire Great Lakes system over millennia.
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Lake Michigan is sinking while Lake Superior's north shore rises, eventually forcing water to flow differently between the lakes in thousands of years.
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The Great Lakes' outlet shifted dramatically when glaciers retreated, causing ancient water to suddenly drain northward into Hudson Bay instead of southward.
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The lakes' drainage reversal happened so fast it created Niagara Falls—a waterfall that's actively eroding backward toward Lake Erie at measurable rates today.
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COMPLETE
Niagara Falls erodes backward roughly one meter per year, meaning it'll reach Lake Erie in about 50,000 years, fundamentally reshaping North America's hydrology.
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