Much of the U.S. West Coast has been tectonically uplifted in the last few million years.

Name: Much of the U.S. West Coast has been tectonically uplifted in the last few million years.
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The U.S. West Coast has experienced significant tectonic uplift over the last few million years, primarily due to the subduction of the Pacific Plate beneath the North American Plate. This uplift has created mountain ranges such as the Sierra Nevada and the Cascade Range.