두코노산
Dukono
복합화산 · Indonesia · 1273m

- 화산 유형
- 복합화산
- 국가
- Indonesia
- 지역
- Western Pacific Volcanic Regions / Halmahera Volcanic Arc
- 해발
- 1273m
- 좌표
- 1.699, 127.878
- 마지막 분화
- 2026년
- 판구조 환경
- Subduction zone / Oceanic crust (< 15 km)
- 화산 지형
- Composite
- 주요 암석
- Andesite / Basaltic Andesite
지질학적 요약
The Dukono complex in northern Halmahera is on an edifice with a broad, low profile containing multiple peaks and overlapping craters. Almost continuous explosive eruptions, sometimes accompanied by lava flows, have occurred since 1933. During a major eruption in 1550 CE, a lava flow filled in the strait between Halmahera and the Gunung Mamuya cone, 10 km NE. Malupang Wariang, 1 km SW of the summit crater complex, contains a 700 x 570 m crater that has also had reported eruptions.
Wikipedia 요약
영어 요약Dukono is an active volcano located in the northern part of Halmahera island, the largest of the Maluku Islands in Indonesia. It has a broad profile and is capped by compound craters. During the major eruption in 1550, a lava flow filled in the strait between Halmahera and the north flank cone of Mount Mamuya. It was an eruption of scale 3 on VEI. Deaths were reported but the figure is unknown. Smaller eruptions occurred in 1719, 1868, and 1901. Since 1933, Dukono has been erupting continuously until the present.
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분화 이력
상세 타임라인
- 1933년VEI 3관측 기록1933-08-13 ~ 2026-03-16Malupang Magiwe and Malupang Warirang
- 1901년VEI 2관측 기록1901 ~ 진행 중
- 1868년VEI 2관측 기록1868 ~ 진행 중
- 1719년 (±150년)VEI ?관측 기록1719 ~ 진행 중East flank of Tolo
- 1550년VEI 3관측 기록1550-11-20 ~ 진행 중
외부 링크
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