La Garita Caldera
||This article includes a list of references, but its sources remain unclear because it has insufficient inline citations. (March 2013)|
|La Garita Caldera|
Ash formations of La Garita Caldera, looking northeast. (Wheeler Geologic Monument)
|Location||Mineral County, Colorado, USA, near Creede|
|Last eruption||26.3 Ma (Fish Canyon Tuff 27.8 Ma)|
La Garita Caldera is a large volcanic caldera located in the San Juan volcanic field in the San Juan Mountains near the town of Creede in southwestern Colorado, United States. It lies to the west of the town of La Garita, Colorado. The eruption that created the La Garita Caldera is the largest known explosive eruption in Earth's history.
The La Garita Caldera is one of a number of calderas that formed during a massive ignimbrite flare-up in Colorado, Utah and Nevada from 40–25 million years ago, and was the site of massive eruptions about 28–26 million years ago, during the Oligocene Epoch.
The area devastated by the La Garita eruption is thought[by whom?] to have covered a significant portion of what is now Colorado, and some research suggests the aerial extent may be as far as the east coast of North America and the Caribbean.
Size of eruption
The scale of La Garita volcanism was one of greatest in recent geologic history. The resulting deposit, known as the Fish Canyon Tuff, has a volume of approximately 1,200 cubic miles (5,000 km3), rating it an 8 on the Volcanic Explosivity Index. This is enough material to fill Lake Michigan. By comparison, the May 18, 1980 eruption of Mt. St. Helens was only 0.25 cubic miles (1.0 km3) in volume. The eruption was energetically equivalent to 240,000 megatons of TNT.
By contrast, the most powerful human-made explosive device ever detonated, the Tsar Bomba or King of the Bombs, had a yield of 50 megatons, whereas the eruption at La Garita was about 5,000 times more powerful. It is one of the most energetic events on Earth since the Chicxulub impact, which was 400 times more powerful than La Garita.
|This section does not cite any references or sources. (April 2013)|
The Fish Canyon Tuff, made of dacite, is uniform in its petrological composition and forms a single cooling unit despite the huge volume. Dacite is a silicic volcanic rock common in explosive eruptions, lava domes and short thick lava flows. There are also large intracaldera lavas composed of andesite, a volcanic rock compositionally intermediate between basalt (poor in silica content) and dacite (higher silica content) in the La Garita Caldera.
The caldera itself, like the eruption of Fish Canyon Tuff, is quite large in scale. It is 35 by 75 kilometers (22 by 47 mi) oblong shape . Most supervolcano calderas of explosive origin are slightly ovoid or oblong in shape. Because of the vast scale and erosion, it took scientists over 30 years to fully determine the size of the caldera. La Garita can be considered a "supervolcano", albeit an extinct one.
La Garita is also the source of at least 7 major eruptions of welded tuff deposits over a time span of 1.5 million years since the Fish Canyon Tuff eruption. The caldera is also known to have extensive outcrops of a very unusual lava-like rock made of dacite that is very similar to that of the Fish Canyon Tuff. This rock, which has characteristics of both lava and welded tuff, was erupted probably shortly before the Fish Canyon Tuff. The lava-like rock has been interpreted as having erupted as thick spatter during low-energy lava fountaining. The lava-like rock is also voluminous — up to 200–300 cubic kilometers (48–72 cu mi).
||This article includes a list of references, but its sources remain unclear because it has insufficient inline citations. (April 2009)|
- Steven, Thomas A.; Peter W. Lipman (1976). "Calderas of the San Juan Volcanic Field, Southwestern Colorado". U.S. Geological Survey Professional Papers (Washington, DC: U.S. Government Printing Office) 958: 1–35. Retrieved 2012, May 16.
- Lipman, Peter W.; Joel E. Robinson, Dillon R. Dutton, David W. Ramsey, and Tracey J. Felger (2006). Geologic Map of the Central San Juan Caldera Cluster, Southwestern Colorado. USGS Geologic Investigations Series I-2799. (includes maps, photo collection, and links to on-line abstracts)
- Ben G. Mason; David M. Pyle, and Clive Oppenheimer (2004). "The size and frequency of the largest explosive eruptions on Earth". Bulletin of Volcanology 66 (8): 735–748. Bibcode:2004BVol...66..735M. doi:10.1007/s00445-004-0355-9.
- Daniel R. Askren; Michael F. Rodden, and James A. Whitney (1997). "Petrogenesis of Tertiary Andesite Lava Flows Interlayered with Large-Volume FelsicAsh-Flow Tuffs of the Western USA" (PDF). Journal of Petrology 38 (8): 1021–1046. doi:10.1093/petrology/38.8.1021. Retrieved 2007-05-02. [dead link]
- Largest explosive eruptions: New results for the 27.8 Ma Fish Canyon Tuff and the La Garita caldera, San Juan volcanic field, Colorado
- The Mid-Tertiary Ignimbrite Flare-Up
- USGS Hawaiian Volcano Observatory: Supersized eruptions are all the rage!
- Robinson, Joel E.; Dillon R. Dutton, David W. Ramsey, Peter W. Lipman, and Tracey J. Felger (2006). Geologic Map of the Central San Juan Caldera Cluster, Southwestern Colorado: Geologic Investigations Series. I-2799. U.S. Geological Survey. Retrieved 2010-05-03.
- "Central Colorado Volcanic field". Journal of Petrology. Retrieved 2010-03-16.
- "Central Colorado Volcanic field". Dr. Matthew E. Brueseke, Department of Geology, Kansas State University. Archived from the original on 2011-07-19. Retrieved 2010-03-26.