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Extent of Lava Creek ash bed.
Tuff Cliff showing the Lava Creek Tuff formation.

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

  1. ^  "Undine Falls, Lava Creek, Yellowstone National Park". Yellowstone Volcano Observatory. http://volcanoes.usgs.gov/yvo/images/20010519-082_caption.html. Retrieved 2005-09-16. 
  2. ^  Lisa Morgan. "Yellowstone Lake Geology Talk Transcript - The floor of Yellowstone Lake is anything but quiet: Volcanic and hydrothermal processes in a large lake above a magma chamber, February 10, 2004". Yellowstone Science Talks. Archived from the original on 2004-05-01. http://web.archive.org/web/20040501035126/http://www.nps.gov/yell/nature/sciencetalks/transcriptmorgan1.htm. Retrieved September 16 2005. 
  3. ^  "U.S. Geological Survey Scientific Investigations Map 2816" (PDF). http://permanent.access.gpo.gov/websites/pubsusgsgovproducts/pubs.usgs.gov/sim/2004/2816/2816_508.pdf. Retrieved September 16 2005. 



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