Global Volcanism Program | Image GVP-02391
Kronotsky is seen here to the NE of the broad summit of Krasheninnikov in the foreground. The slopes of the largely Pleistocene Kronotsky contain deep erosional valleys and had weak phreatic eruptions during the 20th century. Krasheninnikov has been active throughout the Holocene.
Photo by Yuri Doubik (Institute of Volcanology, Petropavlovsk).
This image is made available under the Creative Commons BY-NC 4.0 license terms.