During the Ice Age, glaciers in northern Europe produced proglacial lakes that formed due to the weight of the ice sheets, depressions on the crust, and glacial meltwater.
Glaciers in northern Europe during the Ice Age produced formations known as proglacial lakes. These lakes formed along the edges of the ice sheets due to the depression of the crust under the weight of the glaciers. For example, Lake Agassiz in Manitoba, Canada, and Lake Winnipeg were proglacial lakes that existed along the southern edge of the Laurentide Ice Sheet.
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