The flanks of Kronotsky contain radial erosional valleys up to 200 m deep. The summit, seen here from the north, consists of a basaltic-andesite lava extrusion. The conical, sharp-peaked volcano is one of the most distinctive in Kamchatka.

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

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

Keywords: stratovolcano | erosion

Kronotsky