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Lava Creek Tuff is a tuff formation created when the Yellowstone Caldera erupted about 640,000 years ago.[1] The Lava Creek Tuff distributed in a radial pattern around the caldera and is formed of 1,000 cubic kilometres (240 cu mi) of ash in pyroclastic flows.[2] The tuff has been exposed by erosion at Tuff Cliff along the Gibbon River.[3] Lava Creek Tuff ranges in color from light-gray to pale red in some locales. Density of the tuff ranges from fine-grained to aphanitic and is densely welded. Thickness of the tuff layer ranges from 180–200 m (590–660 ft).[4] [edit] See also[edit] References
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