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Billy Mitchell (volcano)
Crater lake in Bougainville Island From Wikipedia, the free encyclopedia
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Billy Mitchell is a pyroclastic shield, an uncommon type of volcano in the central part of the island of Bougainville, just north-east of the Bagana Volcano in Papua New Guinea. It is a small pyroclastic shield truncated by a 2 km wide caldera filled by a crater lake.[2] It is generally thought to be named after Billy Mitchell, a 20th-century United States Army general who is sometimes regarded as the father of the United States Air Force, although the exact origin of this claim is not known.[3]
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Background
The last two major eruptions were in 1580 AD ± 20 years and about 1030 AD. They were among the largest Holocene eruptions in Papua New Guinea. Both were explosive eruptions with a Volcanic Explosivity Index of at least 5. The 1580 AD ± 20 years eruption produced pyroclastic flows and probably formed its caldera. The second of these eruptions likely had an effect on worldwide temperature, lowering it by 0.2-0.3 degrees celsius for a year or two after the event.[4][5] The ignimbrite deposit from that eruption, which had a VEI of 6, extends 22 kilometres (14 mi) from the caldera to the coast, and its volume is around 10 cubic kilometres (2.4 cu mi).[1]
The volcano is considered dormant as its last eruption was over 350 years ago. [6]
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Caldera lake
Billy Mitchell caldera lake is about 1,013 m above sea level, has a total surface area of 3 km2 (1.2 sq mi), and the maximum depth approximately 88.3 m. The only fish species in the lake is the eel Anguilla megastoma. [7] Billy Mitchell lake drains into the Tekan River.[6]
See also
References
External links
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