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There are no activity reports for Komarov.
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There are no Weekly Reports available for Komarov.
Summary of eruption dates and Volcanic Explosivity Indices (VEI).
|Start Date||Stop Date||Eruption Certainty||VEI||Evidence||Activity Area or Unit|
|0950 (after)||Unknown||Confirmed||Radiocarbon (uncorrected)|
|0450 (?)||Unknown||Confirmed||0||Radiocarbon (uncorrected)|
The following references are the sources used for data regarding this volcano. References are linked directly to our volcano data file. Discussion of another volcano or eruption (sometimes far from the one that is the subject of the manuscript) may produce a citation that is not at all apparent from the title. Additional discussion of data sources can be found under Volcano Data Criteria.
Andreev V I, Litasov N E, Puzankov Y M, 1988. Radioactivity of the basalt-dacite and andesite suites of the Gamchen volcanotectonic structure. Vulc Seism, 7: 219-233 (English translation).
Braitseva O, Ponomareva V, Melekestsev I, Sulerzhitsky L, Pevzner M, 2002-. Holocene Kamchatka volcanoes. http://www.kscnet.ru/ivs/volcanoes/holocene/main/main.htm.
Erlich E N, 1985. . (pers. comm.).
Fedotov S A, Masurenkov Y P (eds), 1991. Active Volcanoes of Kamchatka. Moscow: Nauka Pub, 2 volumes.
IAVCEI, 1973-80. Post-Miocene Volcanoes of the World. IAVCEI Data Sheets, Rome: Internatl Assoc Volc Chemistry Earth's Interior..
Luchitsky I V (ed), 1974. History of the Development of Relief of Siberia and the Far East. Kamchatka, Kurile and Komander Islands. Moscow: Nauka Pub, 439 p (in Russian).
Vlodavetz V I, Piip B I, 1959. Kamchatka and Continental Areas of Asia. Catalog of Active Volcanoes of the World and Solfatara Fields, Rome: IAVCEI, 8: 1-110.
Komarov volcano (also known as Komarova) is a complex structure situated at the northern half of the Gamchen ridge. An eccentric 2.5 x 4 km caldera contains a young twin cone and flank explosive domes. The youngest cone, 2070-m-high Komarov, was built at the western end of the caldera. It is capped by two craters, one at the summit and the other on the upper east flank. Lengthy Holocene lava flows extend beyond the caldera to the east and west. Growth of Komarov volcano began about 1500 years ago following cessation of activity at Visokii volcano. No historical eruptions are known, but the summit region has undergone extensive hydrothermal alteration, and fumarolic areas occur there and on the northern and southern flanks.