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Devils Tower is neither a butte nor a cliff - it is actually an igneous intrusion formed from magma that solidified beneath the Earth's surface. The unique column-like structure that we see today is the result of erosion wearing away the surrounding softer rock, leaving the harder igneous rock exposed.
Devils Tower is a geological feature known as a laccolithic butte, which is a vertical column of igneous rock formed by the solidification of magma below the Earth's surface. It is a significant landmark in northeastern Wyoming, USA.
The address of the Devils Tower Natural History Association is: Po Box 37, Devils Tower, WY 82714-0037
A high flat-topped land form with cliff-like sides that is larger than a butte is a "MESA."
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Devils Tower is a natural geological formation, specifically an igneous intrusion that formed underground and was exposed through erosion. It is not man-made.