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Vysoky

Visokiy

成層火山 · Russia · 1227m

Visokiy (left of center) is surrounded by young lava flows produced by regional basaltic volcanism, seen here from the southwest. Mutnovsky is the cone on the horizon and to the left is Gorely.
Visokiy (left of center) is surrounded by young lava flows produced by regional basaltic volcanism, seen here from the southwest. Mutnovsky is the cone on the horizon and to the left is Gorely. · 写真: Photo by Andrei Tsvetkov, 1977.
タイプ
成層火山
国
Russia
地域
Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
標高
1227m
座標
52.435, 157.933
最終噴火
不明
テクトニクス環境
Subduction zone / Continental crust (> 25 km)
火山地形
Cluster
主要岩石
Basalt / Picro-Basalt
地質学的概要

The basaltic Visokiy cone is the largest and central feature of a 10-km-long line of basaltic cinder cones between Asacha to the SW and Gorely to the NE. The small Golyi shield volcano lies immediately to the WSW (Masurenkov, 1980; Kozhemyaka et al., 1984).

Wikipedia の要約

英語版の要約

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

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噴火履歴

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噴火記録はありません。

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