Dzenzursky

집합화산 · Russia · 2285m

Koryaksky is the tallest peak to the left in the background of this 1990 photo. The ridge to the right of Koryaksky is the eroded Pleistocene age Dzenzursky volcano. This view from the NE has the summit crater rim of Karymsky in the foreground. · 사진: Photo by Dan Miller, 1990 (U.S. Geological Survey). · Wikimedia Commons

화산 유형: 집합화산
국가: Russia
지역: Northwestern Pacific Volcanic Regions / Eastern Kamchatka Volcanic Arc
해발: 2285m
좌표: 53.637, 158.922
마지막 분화: 미확인
판구조 환경: Subduction zone / Continental crust (> 25 km)
화산 지형: Composite
주요 암석: Andesite / Basaltic Andesite

지질학적 요약

Dzenzursky is a strongly eroded stratovolcano of Pleistocene age that lies along a ridge extending NW from Zhupanovsky volcano. A series of Holocene cinder and lava cones along a ridge trending E and SE of the volcano produced extensive lava fields with flows that traveled primarily to the NE. Eruptions were reported in 1923 and 1957 CE (Vlodavetz and Piip 1959, Firstov et al. 1979); however, Fedotov and Masurenkov (1991) did not list any observed eruptions, and Ponomareva (1992, pers. comm.) stated that these reports were of hydrothermal or fumarolic activity.

Wikipedia 요약

영어 요약

Dzenzursky is a stratovolcano located in the southern part of the Kamchatka Peninsula, Russia.

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