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Global Volcanism Program | Image GVP-02393

Kronotsky rises NE of the Kronotsky River, shown across the bottom of the photo. A small cone above the river to the right is one of several on the SW flank. The crater to the lower right is a lake-filled maar that formed at the northern end of a rift zone extending 8 km NNE from Krasheninnikov. The maar erupted along the NE flank of a large Pleistocene caldera inside which Krasheninnikov formed. Photo by Yuri Doubik (Institute of Volcanology, Petropavlovsk).

Kronotsky rises NE of the Kronotsky River, shown across the bottom of the photo. A small cone above the river to the right is one of several on the SW flank. The crater to the lower right is a lake-filled maar that formed at the northern end of a rift zone extending 8 km NNE from Krasheninnikov. The maar erupted along the NE flank of a large Pleistocene caldera inside which Krasheninnikov formed.

Photo by Yuri Doubik (Institute of Volcanology, Petropavlovsk).


Krasheninnikov

Kronotsky