Mount Shiretoko
Shiretoko-Iozan
성층화산 · Japan · 1562m
- 화산 유형
- 성층화산
- 국가
- Japan
- 지역
- Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
- 해발
- 1562m
- 좌표
- 44.133, 145.161
- 마지막 분화
- 1936년
- 판구조 환경
- Subduction zone / Continental crust (> 25 km)
- 화산 지형
- Composite
- 주요 암석
- Andesite / Basaltic Andesite
지질학적 요약
Shiretoko-Iozan, one of many Japanese "sulfur mountains," is noted for the extrusion of molten sulfur during eruptions in 1889 and 1936. Located at the NE tip of Hokkaido on the Shiretoko Peninsula, the andesitic volcano contains two large craters at the summit that are breached to the NW. The southern crater contains a small flat-topped lava dome. The main cone, Nakadake, was constructed NW of the headwalls of the two breached craters. Historical eruptions have originated from the southernmost of three explosion craters along a NNE-SSW line on the NW flank of the main cone.
Wikipedia 요약
영어 요약Mount Shiretoko is a volcano located on the Shiretoko Peninsula in Hokkaido, Japan. The mountain consists of non-alkali mafic rocks and andesite. Mount Shiretoko is in Shari town, in Shari District of Okhotsk Subprefecture.
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분화 이력
상세 타임라인
- 1935년VEI 1관측 기록1935-12 ~ 1936-10NW flank
- 1890년VEI 1관측 기록1890-06-15 ~ 진행 중NW flank
- 1889년VEI 2관측 기록1889-08-09 ~ 1889-10-07NW flank
- 1880년VEI ?지질학적 추정1880-11-24 ~ 1880-11-26
- 1876년VEI 2관측 기록1876-09-23 ~ 1876-09-26NW flank
- 1857년VEI ?관측 기록1857 ~ 1858
- 850년 (±500년)VEI ?지질학적 추정850 ~ 진행 중
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