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Global Volcanism Program | Image GVP-10808

Stokap (center) lies at the SW end of Nishihitokappuyama, an elongated chain of small volcanoes on southern Iturup Island. Nishihitokappuyama consists of a cluster of small NE-SW-trending late-Pleistocene to Holocene cones and craters. Stokap contains 8-10 cones and craters, the largest of which contains a lake. The flank of Etorofu-Atosanupuri is seen in the foreground. Photo by Alexander Rybin, 2001 (Institute of Marine Geology and Geophysics, Yuzhno-Sakhalin).

Stokap (center) lies at the SW end of Nishihitokappuyama, an elongated chain of small volcanoes on southern Iturup Island. Nishihitokappuyama consists of a cluster of small NE-SW-trending late-Pleistocene to Holocene cones and craters. Stokap contains 8-10 cones and craters, the largest of which contains a lake. The flank of Etorofu-Atosanupuri is seen in the foreground.

Photo by Alexander Rybin, 2001 (Institute of Marine Geology and Geophysics, Yuzhno-Sakhalin).

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Keywords: stratovolcano


Hitokappu Volcano Group [Bogatyr Ridge]