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Yarmouthian


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The second (0.23–0.17 Ma) of four interglacial stages recognized in mid-continental North America. It follows the Kansan glacial episode and is equivalent to the upper part of the Günz/Mindel Interglacial of the Alps. At various times during the Yarmouthian climates were both warmer and cooler than they are now.

Subjects: Ecology and Conservation — Earth Sciences and Geography.


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