Dzenzursky

Gunung api majemuk · Russia · 2285 m

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. · Foto: Photo by Dan Miller, 1990 (U.S. Geological Survey). · Wikimedia Commons

Tipe: Gunung api majemuk
Negara: Russia
Wilayah: Northwestern Pacific Volcanic Regions / Eastern Kamchatka Volcanic Arc
Ketinggian: 2285 m
Koordinat: 53.637, 158.922
Letusan terakhir: Tidak diketahui
Kondisi tektonik: Subduction zone / Continental crust (> 25 km)
Bentuk lahan: Composite
Batuan utama: Andesite / Basaltic Andesite

Ringkasan geologi

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.

Ringkasan Wikipedia

Ringkasan Inggris

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

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