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The ice ages significantly shaped the landscape of North America. The massive ice sheets that covered large parts of the continent exerted enormous pressure on the land, carving out valleys, altering the course of rivers, and creating many of the Great Lakes. As the ice sheets retreated, they left behind a variety of geological features, including moraines, drumlins, and kettle lakes.
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During the 1800s, scientists came to the consensus that the Earth had experienced a number of ice ages in which large parts of the planet had been covered in ice sheets. During the last glacial maximum, the location of what is now Boston had more than a full kilometer of ice above it. Toronto had two kilometers. Montréal had more than three. The southernmost edges of the North American ice sheet were in northern Kentucky and West Virginia.
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