일본 · 성층화산
오소레야마 산
Osorezan
- 화산 유형
- 성층화산
- 해발
- 878m
- 마지막 분화
- 1787년

- 화산 유형
- 성층화산
- 국가
- 일본
- 지역
- 북서태평양 / Northeast Japan Volcanic Arc
- 해발
- 878m
- 좌표
- 41.279, 141.120
- 마지막 분화
- 1787년
- 판구조 환경
- 섭입대 / 대륙 지각 (> 25 km)
- 화산 지형
- 복성화산체
- 주요 암석
- 안산암 / 현무암질 안산암
지질학적 요약
Osorezan, on the Shimokita Peninsula in northernmost Honshu, contains a 5-km-wide caldera partly occupied by a shallow lake that drains through the N caldera wall. Dissected lava domes ring the caldera floor. The andesitic-to-dacitic volcano is largely Pleistocene in age, with activity dating back about 800,000 years. The last identified distal tephra deposit was erupted during the late Pleistocene. The only report of historical activity was in a Tohoku district travel document published in 1787, which stated that Yakeyama in Mutsu country (Osoreyama) had erupted. Older residents reported that large fires and clouds were sometimes seen from the summit, accounting for the volcano's local name, Yakeyama, or "Burning Mountain" (Murayama, 1987). Earthquake swarms have been documented during the second half of the 20th century, and magma bodies have been detected beneath the volcano.
Wikipedia 요약
영어 요약Mount Osore is the name of a Buddhist temple and folk religion pilgrimage destination in the center of remote Shimokita Peninsula of Aomori Prefecture, in the northern Tōhoku region of northern Japan. The temple is located in the caldera of an active volcano and is believed in Japanese mythology to be one of the gates to the underworld.
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분화 이력
1건 기록용어집상세 타임라인
- 1787년VEI ?관측 기록1787 ~ 종료일 미상
주변 화산
외부 링크
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