시바약산
Singkut
칼데라 · Indonesia · 2181m
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- 화산 유형
- 칼데라
- 국가
- Indonesia
- 지역
- 순다·반다 / Sunda Volcanic Arc
- 해발
- 2181m
- 좌표
- 3.238, 98.513
- 마지막 분화
- 1881년
- 판구조 환경
- Subduction zone / Continental crust (> 25 km)
- 화산 지형
- Caldera
- 주요 암석
- Andesite / Basaltic Andesite
지질학적 요약
The Quaternary Singkut caldera is about 7 x 4 km with the S half of the rim topographically distinct. Post-caldera cones have filled much of the crater and the N rim, including Sibayak, Pintau, and Pratektekan. The 900-m-wide Sibayak crater is partially filled on the north by Pintau. A lava flow traveled through a gap in the western crater wall from the summit lava dome of Sibayak; the active geothermal field SE of the summit has abundant solfataras and fumaroles. Area residents record legends of eruptions. Neumann van Padang (1983) cited a report by Hoekstra of ash clouds emitted from the volcano in 1881. The town of Berastagi is within the caldera immediately SE of the younger cones.
Wikipedia 요약
영어 요약Mount Sibayak is a stratovolcano overlooking the town of Berastagi in northern Sumatra, Indonesia. Although its last eruption was more than a century ago, geothermal activity in the form of steam vents and hot springs remains high on and around the volcano. The vents produce crystalline sulfur, which was mined on a small scale in the past. Seepage of sulfurous gases has also caused acidic discolouration of the small crater lake.
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분화 이력
상세 타임라인
- 1881년VEI ?관측 기록1881-07-02 ~ 진행 중
외부 링크
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