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Global Volcanism Program | Image GVP-02363

Maly Semiachik, seen here from the SW on the flanks of Karymsky, is composed of three overlapping edifices along a NW-SE line that were built within two overlapping Pleistocene calderas. The late-Pleistocene to Holocene post-caldera massif almost completely obscures the rim of the inner 7-km-wide Maly Semiachik caldera.  Photo by Dan Miller, 1990 (U.S. Geological Survey).

Maly Semiachik, seen here from the SW on the flanks of Karymsky, is composed of three overlapping edifices along a NW-SE line that were built within two overlapping Pleistocene calderas. The late-Pleistocene to Holocene post-caldera massif almost completely obscures the rim of the inner 7-km-wide Maly Semiachik caldera.

Photo by Dan Miller, 1990 (U.S. Geological Survey).

Keywords: stratovolcano


Maly Semyachik