During the Pleistocene epoch,continental glaciers alternately advanced and retreated over large portions of North America and Europe.

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The Pleistocene epoch, which began about 2.6 million years ago and ended about 11,700 years ago, was characterized by multiple glaciations that caused the advance and retreat of continental glaciers over large parts of North America and Europe. This led to the formation of various landforms, such as moraines, glacial lakes, and outwash plains, that still exist today.

During the Pleistocene Epoch,continental Glaciers Alternately Advanced and Retreated Over