Mountain Sumbing
Sumbing
성층화산 · Indonesia · 3370m
- 화산 유형
- 성층화산
- 국가
- Indonesia
- 지역
- Sunda-Banda Volcanic Regions / Sunda Volcanic Arc
- 해발
- 3370m
- 좌표
- -7.382, 110.075
- 마지막 분화
- 1730년
- 판구조 환경
- Subduction zone / Continental crust (> 25 km)
- 화산 지형
- Composite
- 주요 암석
- Andesite / Basaltic Andesite
지질학적 요약
Gunung Sumbing is a stratovolcano that is the SE-most edifice of a chain of volcanoes in central Java that includes Sundoro and the Dieng Complex. Prominent cones are located on the N and SE flanks. An 800-m-wide summit crater is breached to the NE, but is partially filled by a lava dome that extended beyond the original crater rim. Emplacement of the dome followed the production of extensive pyroclastic flows down the NE flank. Activity reported in about 1730 CE may have produced the small phreatic craters found at the summit behind the dome.
Wikipedia 요약
영어 요약Mount Sumbing is an active stratovolcano in Central Java, Indonesia. This volcano is symmetrical like its neighbor Mount Sindoro which lies to its northwest. Administratively, The volcano is divided between 3 regencies: Temanggung, Wonosobo, and Magelang. The only report of historical eruptions is from 1730. It has created a small phreatic crater at the summit.
Wikipedia · CC BY-SA · 전체 기사 보기 →
분화 이력
상세 타임라인
- 1730년VEI 1관측 기록1730 ~ 진행 중
외부 링크
⚠ 참고용 정보입니다. 재난 대응에 사용하지 마세요.