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Global Volcanism Program | Image GVP-02397

Tolbachik is composed of two main edifices. The flat-topped Plosky Tolbachik (right) is located east of the older and higher Ostry Tolbachik cone (left). Lengthy rift zones extending NE and S of Plosky Tolbachik have erupted voluminous lava flows through the Holocene. The 1975-76 eruption from the summit and S-flank fissures was one of the largest historical basaltic eruption in Kamchatka. Photo by Oleg Volynets (Institute of Volcanology, Petropavlovsk).

Tolbachik is composed of two main edifices. The flat-topped Plosky Tolbachik (right) is located east of the older and higher Ostry Tolbachik cone (left). Lengthy rift zones extending NE and S of Plosky Tolbachik have erupted voluminous lava flows through the Holocene. The 1975-76 eruption from the summit and S-flank fissures was one of the largest historical basaltic eruption in Kamchatka.

Photo by Oleg Volynets (Institute of Volcanology, Petropavlovsk).

Creative Commons Icon This image is made available under the Creative Commons BY-NC 4.0 license terms.

Keywords: stratovolcano


Tolbachik