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카위산

Kawi-Butak

성층화산 · Indonesia · 2651m

The broad Kawi-Butak volcanic massif rises above rice paddies below its SW flank. The forested volcano lies immediately east of Kelud volcano and south of Arjuno-Welirang volcano. The high point of the complex is flat-topped Gunung Butak on the right horizon. Gunung Kawi (left-center) was constructed to the NW of Butak. Both are primarily of Holocene age.
The broad Kawi-Butak volcanic massif rises above rice paddies below its SW flank. The forested volcano lies immediately east of Kelud volcano and south of Arjuno-Welirang volcano. The high point of the complex is flat-topped Gunung Butak on the right horizon. Gunung Kawi (left-center) was constructed to the NW of Butak. Both are primarily of Holocene age. · 사진: Photo by Lee Siebert, 2000 (Smithsonian Institution). · Wikimedia Commons
화산 유형
성층화산
국가
Indonesia
지역
Sunda-Banda Volcanic Regions / Sunda Volcanic Arc
해발
2651m
좌표
-7.920, 112.450
마지막 분화
미확인
판구조 환경
Subduction zone / Continental crust (> 25 km)
화산 지형
Composite
주요 암석
No Data (checked)
지질학적 요약

The broad Kawi-Butak volcanic massif lies immediately E of Kelut volcano and S of Arjuno-Welirang volcano. Gunung Kawi was constructed to the NW of Gunung Butak. No historical eruptions are known from either volcano, but both are primarily of Holocene age.

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