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운젠산

Unzendake

복합화산 · Japan · 1483m

The Unzen volcanic complex comprises much of the Shimabara Peninsula east of Nagasaki, seen here looking to the W from across Shimabara Bay. Three large edifices are visible: Kinugasa to the N, Fugendake in the E-center, and Kusenbu on the S. Historical eruptive activity has occurred at the summit and flanks of Fugendake. Activity during 1990-95 formed a lava dome at the summit that produced pyroclastic flows (block-and-ash flows).
The Unzen volcanic complex comprises much of the Shimabara Peninsula east of Nagasaki, seen here looking to the W from across Shimabara Bay. Three large edifices are visible: Kinugasa to the N, Fugendake in the E-center, and Kusenbu on the S. Historical eruptive activity has occurred at the summit and flanks of Fugendake. Activity during 1990-95 formed a lava dome at the summit that produced pyroclastic flows (block-and-ash flows). · 사진: Photo by Tom Casadevall, 1991 (U.S. Geological Survey). · Wikimedia Commons
화산 유형
복합화산
국가
Japan
지역
서태평양 / Nankai Volcanic Arc
해발
1483m
좌표
32.761, 130.299
마지막 분화
1996년
판구조 환경
Subduction zone / Continental crust (> 25 km)
화산 지형
Composite
주요 암석
Andesite / Basaltic Andesite
지질학적 요약

The massive Unzendake volcanic complex comprises much of the Shimabara Peninsula east of the city of Nagasaki. An E-W graben, 30-40 km long, extends across the peninsula. Three large stratovolcanoes with complex structures, Kinugasa on the north, Fugen-dake at the east-center, and Kusenbu on the south, form topographic highs on the broad peninsula. Fugendake and Mayuyama volcanoes in the east-central portion of the andesitic-to-dacitic volcanic complex have been active during the Holocene. The Mayuyama lava dome complex, located along the eastern coast west of Shimabara City, formed about 4000 years ago and was the source of a devastating 1792 CE debris avalanche and tsunami. Historical eruptive activity has been restricted to the summit and flanks of Fugendake. The latest activity during 1990-95 formed a lava dome at the summit, accompanied by pyroclastic flows that caused fatalities and damaged populated areas near Shimabara City.

분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
4050 BCE~3848 BCE · 1건 · 최고 VEI ?2841 BCE~2639 BCE · 2건 · 최고 VEI ?2236 BCE~2035 BCE · 1건 · 최고 VEI ?1632 BCE~1430 BCE · 1건 · 최고 VEI ?1229 BCE~1027 BCE · 1건 · 최고 VEI ?787~988 · 1건 · 최고 VEI ?1593~1794 · 4건 · 최고 VEI 21794~1996 · 3건 · 최고 VEI 24050 BCE2639 BCE1027 BCE3841794

상세 타임라인

  1. 1996년VEI 2관측 기록
    1996-02-10 ~ 1996-05-01
    Fugen-dake
  2. 1990년VEI 1관측 기록
    1990-11-17 ~ 1995-02-16
    Fugen-dake
  3. 1798년VEI ?지질학적 추정
    1798-11-13 ~ 1798-12
    Fugen-dake
  4. 1792년VEI 2관측 기록
    1792-02-10 ~ 1792-07-22
    Fugen-dake (summit, NNE), Mayu-yama
  5. 1690년VEI ?지질학적 추정
    1690 ~ 1692
  6. 1663년VEI 2관측 기록
    1663-04 ~ 1663-05
    Fugen-dake (Tsukumo-jima Pond)
  7. 1663년VEI 2관측 기록
    1663-12-11 ~ 1663-12-27
    NE flank of Fugen-dake (1200 m)
  8. 860년VEI ?지질학적 추정
    860 ~ 진행 중
  9. 기원전 1150년 (±500년)VEI ?지질학적 추정
    BCE 1150 ~ 진행 중
    Fugendake-Sancho
  10. 기원전 1450년 (±500년)VEI ?지질학적 추정
    BCE 1450 ~ 진행 중
    Fugen-dake (Kazaana)
  11. 기원전 2150년 (±800년)VEI ?지질학적 추정
    BCE 2150 ~ 진행 중
    Mayu-yama (Tengu-yama)
  12. 기원전 2640년 (±500년)VEI ?지질학적 추정
    BCE 2640 ~ 진행 중
    Mayu-yama (Shichimen-zan)
  13. 기원전 2720년 (±300년)VEI ?지질학적 추정
    BCE 2720 ~ 진행 중
    Fugen-dake
  14. 기원전 4050년 (±3000년)VEI ?지질학적 추정
    BCE 4050 ~ 진행 중
    Fugen-dake (Shimanomine)

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