Mount Tongkoko
Tangkoko-Duasudara
성층화산 · Indonesia · 1334m

- 화산 유형
- 성층화산
- 국가
- Indonesia
- 지역
- Western Pacific Volcanic Regions / Sangihe Volcanic Arc
- 해발
- 1334m
- 좌표
- 1.518, 125.185
- 마지막 분화
- 1880년
- 판구조 환경
- Subduction zone / Continental crust (> 25 km)
- 화산 지형
- Composite
- 주요 암석
- Andesite / Basaltic Andesite
지질학적 요약
The eastern peninsula at the far NE end of Sulawesi near the city of Bitung is occupied by a volcanic complex consisting of two major edifices within a nature reserve. To the north is Tangkoko (also known as Tongkoko), with a large caldera (~3 x 1.5 km) elongated towards the SE from the highest rim point; the rim at the opposite end is more than 400 m lower. Eruptions occurred from the summit crater in the 17th century and in 1801, when the caldera also reportedly contained a cone surrounded by a lake. About 1.5 km down the outer E flank is the Batuangus (or Batu Angus) lava dome, formed in 1801, along with an adjacent vent (Baru Batuangus) that has been the source of all subsequent eruptions. The higher Duasudara (also Dua Suadara) edifice is ~4.5 km SW of the Tangkoko summit. A NE-facing scarp appears to have a hummocky debris flow that reaches the base of Tangkoko.
분화 이력
상세 타임라인
- 1880년VEI 1관측 기록1880 ~ 진행 중Batu Angus
- 1843년VEI 2관측 기록1843 ~ 1846Batu Angus
- 1821년VEI 0관측 기록1821 ~ 진행 중Batu Angus Baru
- 1801년VEI 2관측 기록1801 ~ 진행 중Summit and east flank (Batu Angus)
- 1694년VEI 3관측 기록1694 ~ 진행 중
- 1683년VEI 3관측 기록1683 ~ 진행 중
- 1680년VEI 5관측 기록1680 ~ 진행 중
외부 링크
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