Much of the rich loess of the central plains of the United States is the result of the Pleistocene Ice Age.

Name: Much of the rich loess of the central plains of the United States is the result of the Pleistocene Ice Age.
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During the Pleistocene Ice Age, glaciers formed and melted several times, depositing huge amounts of sediment and creating the rich loess soil of the central plains of the United States.

Much of the Rich Loess of the Central Plains of the United