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아우산

Awu

성층화산 · Indonesia · 1318m

A shallow lake partially fills the summit crater of Awu volcano in this 1995 view.  Gunung Awu volcano, one of the deadliest in Indonesia, is cut by deep valleys that form passageways for lahars dissect the flanks of the 1320-m-high volcano.  Powerful explosive eruptions in 1711, 1812, 1856, 1892, and 1966 produced devastating pyroclastic flows and lahars that caused more than 8000 fatalities.
A shallow lake partially fills the summit crater of Awu volcano in this 1995 view. Gunung Awu volcano, one of the deadliest in Indonesia, is cut by deep valleys that form passageways for lahars dissect the flanks of the 1320-m-high volcano. Powerful explosive eruptions in 1711, 1812, 1856, 1892, and 1966 produced devastating pyroclastic flows and lahars that caused more than 8000 fatalities. · 사진: Photo by Kristianto, 1995 (Centre of Volcanology & Geological Hazard Mitigation, Volcanological Survey of Indonesia). · Wikimedia Commons
화산 유형
성층화산
국가
Indonesia
지역
Western Pacific Volcanic Regions / Sangihe Volcanic Arc
해발
1318m
좌표
3.689, 125.447
마지막 분화
2004년
판구조 환경
Subduction zone / Oceanic crust (< 15 km)
화산 지형
Composite
주요 암석
Andesite / Basaltic Andesite
지질학적 요약

The massive Gunung Awu stratovolcano occupies the northern end of Great Sangihe Island, the largest of the Sangihe arc. Deep valleys that form passageways for lahars dissect the flanks of the volcano, which was constructed within a 4.5-km-wide caldera. Powerful explosive eruptions in 1711, 1812, 1856, 1892, and 1966 produced devastating pyroclastic flows and lahars that caused more than 8000 cumulative fatalities. Awu contained a summit crater lake that was 1 km wide and 172 m deep in 1922, but was largely ejected during the 1966 eruption.

Wikipedia 요약

영어 요약

Mount Awu is the largest stratovolcano in the Sangihe Islands chain, located on Sangir Island in North Sulawesi, Indonesia. Powerful eruptions have occurred in 1711, 1812, 1856, 1822, 1892, and 1966 with devastating pyroclastic flows and lahars that resulted in 11,048 fatalities. A total of 18 eruptions are recorded from 1640, with two of VEI 4 and 3 with VEI 3, one eruption every ~ 20 years. The hazardous nature of the volcano is determined from the continuous lava source driven by the geodynamic setting and the presence of a crater lake, sustained by the consistent rainfall on the island, on top of a lava dome. This setting creates the conditions for water injection in the lava dome, which can cause a water-magma explosion.

Wikipedia · CC BY-SA · 전체 기사 보기

분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
1640~1676 · 2건 · 최고 VEI 31676~1713 · 2건 · 최고 VEI 31786~1822 · 1건 · 최고 VEI 41822~1858 · 1건 · 최고 VEI 31858~1895 · 5건 · 최고 VEI 31895~1931 · 4건 · 최고 VEI 21931~1968 · 1건 · 최고 VEI 41968~2004 · 3건 · 최고 VEI 216401713182218951968

상세 타임라인

  1. 2004년VEI 2관측 기록
    2004-06-02 ~ 2004-08-16
  2. 1992년VEI 1관측 기록
    1992-04-07 ~ 진행 중
    SE part of summit crater
  3. 1968년VEI 2지질학적 추정
    1968-08-16 ~ 1968-09-16
  4. 1966년VEI 4관측 기록
    1966-08-12 ~ 1966-10-16
  5. 1930년VEI 2관측 기록
    1930-12 ~ 1931-12
  6. 1922년VEI 0관측 기록
    1922-06-20 ~ 1922-09
  7. 1921년VEI 0관측 기록
    1921-02 ~ 1921-10-01
  8. 1913년VEI 2관측 기록
    1913-03-14 ~ 1913-03-14
  9. 1893년VEI 2관측 기록
    1893 ~ 진행 중
  10. 1892년VEI 3관측 기록
    1892-06-07 ~ 1892-06-12
  11. 1885년VEI 2관측 기록
    1885-08-18 ~ 진행 중
  12. 1883년VEI 2관측 기록
    1883-08-25 ~ 1883-08-26
  13. 1875년VEI 2관측 기록
    1875-08 ~ 1875-08
  14. 1856년VEI 3관측 기록
    1856-03-02 ~ 1856-03-17
  15. 1812년VEI 4관측 기록
    1812-08-06 ~ 1812-08-08
  16. 1711년VEI 3관측 기록
    1711-12-10 ~ 1711-12-16
  17. 1699년VEI ?지질학적 추정
    1699 ~ 진행 중
  18. 1646년 (±5년)VEI 2관측 기록
    1646 ~ 진행 중
  19. 1640년VEI 3지질학적 추정
    1640-12 ~ 1641-01-04

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