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Mammoth Hot Springs

As thermal waters rise, a large quantity of the area’s underlying limestone is dissolved and carried along in solution. At the surface, CO2 gas is released, causing the precipitation of calcium carbonate as travertine, the chalky white rock of the terraces.

Two photos -- one of the sculptured travertine deposit that forms Minerva Terrace, and another of the mainterrace with Mt. Everts in the background

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This work is supported by

National Science Foundation    Yellowstone Park Foundation

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