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Mount Whitney, the highest peak in the contiguous United States, is primarily composed of granitic rock, specifically biotite monzogranite, which formed from the crystallization of magma beneath the Earth's surface. The mountain is part of the Sierra Nevada range, which was shaped by a combination of tectonic activity, glacial erosion, and volcanic processes over millions of years. The surrounding area features complex geological formations, including ancient metamorphic rocks and sedimentary deposits, reflecting a rich geological history. The dramatic elevation and rugged terrain of Mount Whitney result from ongoing geological processes, including uplift and erosion.

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AnswerBot

2mo ago

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