Medvezhya
Moyorodake [Medvezhia]
성층화산 · Japan - administered by Russia · 1124m
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- 화산 유형
- 성층화산
- 국가
- Japan - administered by Russia
- 지역
- Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
- 해발
- 1124m
- 좌표
- 45.389, 148.838
- 마지막 분화
- 1999년
- 판구조 환경
- Subduction zone / Intermediate crust (15-25 km)
- 화산 지형
- Composite
- 주요 암석
- Andesite / Basaltic Andesite
지질학적 요약
The Moyorodake volcanic complex (also known as Medvezhia) occupies the NE end of Iturup (Etorofu) Island. Two overlapping calderas, 14 x 18 and 10 x 12 km in diameter, were formed during the Pleistocene. The caldera floor contains several lava domes, cinder cones and associated lava fields, and a small lake. Four small closely spaced stratovolcanoes were constructed along an E-W line on the eastern side of the complex. The easternmost and highest, Medvezhii, lies outside the western caldera, along the Pacific coast. Srednii, Tukap, and Kudriavy (Moyorodake) volcanoes lie immediately to the west. Historically active Moyorodake is younger than 2000 years; it and Tukap remain fumarolically active. The westernmost of the post-caldera cones, Menshoi Brat, is a large lava dome with flank scoria cones, one of which has produced a series of young lava flows up to 4.5 km long that reached Slavnoe Lake. Eruptions have been documented since the 18th century, although lava flows from cinder cones on the flanks of Menshoi Brat were also probably erupted within the past few centuries.
Wikipedia 요약
영어 요약Medvezhya (Russian: Медве́жий вулкан; Japanese: 茂世路岳, Moyoro-dake) is a volcanic complex located at the northern end of Iturup Island, Kuril Islands, Russia. Rheniite, a rhenium sulfide mineral (ReS2), was discovered within the active hot fumaroles of the volcano in 1994
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분화 이력
상세 타임라인
- 1999년VEI 1관측 기록1999-10-07 ~ 1999-10-13Kudriavy
- 1958년VEI 1관측 기록1958-07-02 ~ 진행 중Kudriavy
- 1946년VEI 2지질학적 추정1946 ~ 진행 중Kudriavy
- 1883년VEI 2관측 기록1883-05 ~ 1883-06Kudriavy
- 1778년VEI 2관측 기록1778-12-31 ~ 진행 중Kudriavy
- 기원전 50년VEI ?지질학적 추정BCE 50 ~ 진행 중
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