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Geological Formations

El Capitan

Inselbergs and Crystalline Monoliths

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El Capitan is a vertical granite monolith rising about 900 meters from the floor of Yosemite Valley in the Sierra Nevada of California, formed from the El Capitan Granite, part of the Sierra Nevada Batholith, a vast body of magma that intruded and slowly crystallized deep underground between roughly 130 and 100 million years ago. Its sheer face is largely the product of glacial erosion: repeated glaciations during the last two million years carved and steepened Yosemite Valley, plucking away jointed and fractured granite along the valley walls to leave the exceptionally smooth, uninterrupted cliff face for which El Capitan is renowned. The rock's minimal jointing and fracturing, unusual for granite, gives it the continuous, unbroken vertical expanse that has made it one of the most celebrated big-wall rock climbing formations in the world.

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Glaciation, Processes

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