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아이슬란드 · 순상화산

Þeistareykjarbunga

Theistareykir

화산 유형
순상화산
해발
563m
마지막 분화
-900년
Stóravíti crater, seen here from the SE, is 600 m across and 140 m deep. It is located in the summit area of the Holocene Theistareykjarbunga shield volcano, part of the northernmost subaerial volcanic system along the Eastern Volcanic Zone of Iceland. The youngest dated eruption in this system produced the Theistareykjahraun lava flow about 2,400 years ago.
Stóravíti crater, seen here from the SE, is 600 m across and 140 m deep. It is located in the summit area of the Holocene Theistareykjarbunga shield volcano, part of the northernmost subaerial volcanic system along the Eastern Volcanic Zone of Iceland. The youngest dated eruption in this system produced the Theistareykjahraun lava flow about 2,400 years ago. · 사진: Photo by Michael Ryan, 1984 (U.S. Geological Survey).
화산 유형
순상화산
국가
아이슬란드
지역
대서양 / Iceland Neovolcanic Rift Volcanic Province
해발
563m
좌표
65.883, -16.967
마지막 분화
-900년
판구조 환경
열곡대 / 해양 지각 (< 15 km)
화산 지형
순상화산체
주요 암석
현무암 / 피크로현무암
지질학적 요약

The Holocene Theistareykir fissure system, including the basaltic Theistareykjarbunga shield volcano, extends from north of Myvatn lake to the coast of Iceland. This is the northernmost subaerial volcanic system along the Eastern Volcanic Zone of Iceland. The 30 km3 Theistareykjarbunga shield volcano formed slightly after deglaciation; the youngest dated eruption produced the Theistareykjahraun lava flow about 2,400 years ago.

Wikipedia 요약

영어 요약

Theistareykjarbunga is a shield volcano in north-eastern Iceland with two fissure vents called Þeistareykjahraun and Borgahraun, and two cones: the 370 m (1,210 ft) Stórahversmór and the 540 m (1,770 ft), 30 km3 (7.2 cu mi) Stóravíti. They both are currently extinct, although there is evidence suggesting the potential for activity such as recent localised uplift and seismicity. The multiple vents make up the Theistareykir (Þeistareykir) volcanic system, with more recent evidence that the former classification as a shield volcano is better considered an embryonic central volcano with associated fissure swarm, as rhyolite has erupted in a limited area. The recent lava has picrite, olivine tholeiite basalt characteristics but before the ice age there were basaltic andesite and rhyolite eruptions. There is a central high temperature geothermal area with numerous steam vents and fumaroles. This has been utilised by a 90 MWe power station.

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분화 이력

3건 기록용어집
요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다 · 화살표 키로 막대 이동, Enter로 열기
기원전 9500~기원전 9213 · 1건 · 최고 VEI 0기원전 6920~기원전 6633 · 1건 · 최고 VEI 0기원전 1187~기원전 900 · 1건 · 최고 VEI 0기원전 9500기원전 7493기원전 5200기원전 3193기원전 1187

상세 타임라인

  1. 기원전 900년 (±100년)VEI 0지질학적 추정
    기원전 900 ~ 종료일 미상
    Storihver (Theistareykjahraun)
  2. 기원전 6800년VEI 0지질학적 추정
    기원전 6800 ~ 종료일 미상
    Borgarhraun and other flows
  3. 기원전 9500년VEI 0지질학적 추정
    기원전 9500 ~ 종료일 미상
    Theistareykjabunga shield volcano

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