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Hydrothermal Research

TRAVERTINE AND GEYSERITE

A travertine terrace Travertine
Underlying bedrock: Limestone (sedimentary)
Composition: Calcium carbonate
How is it deposited? Warm, carbon dioxide-rich waters dissolve calcium carbonate from the underlying bedrock. The calcium carbonate precipitates out of solution when the carbon dioxide is released.
Usual rate of deposition: Rapid

A photo of geyserite Geyserite
Underlying bedrock: Rhyolite (volcanic)
Composition: Silica
How is it deposited? Superheated water dissolves silica from the underlying bedrock. Geyser water splashes onto the ground, forming hard, translucent, bulbous, or spiny shapes called geyserite.
Usual rate of deposition: very slowly—perhaps only an inch or two in a hundred years.

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This work is supported by

National Science Foundation    Yellowstone Park Foundation
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