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Example of the formation of a caldera, the pictures show Mount Mazama's eruption timeline
Crater Lake in Oregon

A caldera is a volcanic feature formed by the collapse of land surface after a gigantic volcanic eruption. In such an eruption the volcano's magma chamber is empty enough for the ground above it to drop.[1]

A caldera may look like a volcanic crater except that a crater is made by blasting outward, not by collapsing inward.[2] The word caldera comes from the Portuguese language, meaning "cauldron". Some complex features are made by both processes.

When Yellowstone Caldera last erupted some 650,000 years ago, it released about 1,000 km3 of material, covering much of North America in debris up to two metres thick. By comparison, when Mount St. Helens erupted in 1980, it released 1000 times less material.

The ecological effects of the eruption of a large caldera can be seen in the record of the Lake Toba eruption in Indonesia.

About 75,000 years ago, the Toba catastrophe released about 2,800 km3 of ejecta. This was the largest known explosive eruption within the last 25 million years. In the late 1990s, anthropologist Stanley Ambrose suggested that a volcanic winter induced by this eruption reduced the human population to about 2,000 – 20,000, resulting in a population bottleneck.[3] Others suggested that the human race was reduced to about five to ten thousand people.[4] However, there is no direct evidence that the theory is correct [5] and some evidence that it is not.[6]

Larger calderas[change | change source]

Eruptions forming even larger calderas are known. At La Garita Caldera in the San Juan Mountains of Colorado, the 5,000 km3 Fish Canyon Tuff was blasted out in a single major eruption about 27.8 million years ago.

At some points in time, rhyolitic calderas have appeared in distinct clusters. The remnants of such clusters may be found in places such as the San Juan Mountains of Colorado (formed during the Oligocene, Miocene, and Pliocene periods) or the Saint Francois Mountain Range of Missouri (erupted during the Proterozoic).

Satellite image of Santorini. Clockwise from center: Nea Kameni; Palea Kameni; Aspronisi; Therasia; Thera

References[change | change source]

  1. Francis, Peter 1993. Volcanoes: a planetary perspective. Oxford University Press. Chapter 14, p291 et seq. ISBN 0-19-854033-7
  2. "Glossary of Terms: C". Retrieved 2008-04-12.
  3. "Professor Stanley H Ambrose PhD | Anthropology at Illinois". Retrieved 2017-12-06.
  4. Supervolcanoes, BBC2, 3 February 2000
  5. Gathorne-Hardy F.J. & Harcourt-Smith W.E.H. 2003. The super-eruption of Toba: did it cause a human bottleneck? Journal of Human Evolution. 45, 227-230
  6. Petraglia M et al. 2007. "Middle Paleolithic assemblages from the Indian subcontinent before and after the Toba super-eruption" Archived 2016-03-03 at the Wayback Machine. Science 317 (5834): 114–116. doi:10.1126/science.1141564. PMID 17615356.