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The Global Volcanism Program has no activity reports for Komarov.
The Global Volcanism Program has no Weekly Reports available for Komarov.
The Global Volcanism Program has no Bulletin Reports available for Komarov.
Summary of Holocene 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)|
This compilation of synonyms and subsidiary features may not be comprehensive. Features are organized into four major categories: Cones, Craters, Domes, and Thermal Features. Synonyms of features appear indented below the primary name. In some cases additional feature type, elevation, or location details are provided.
|Zapovedny | Komarova|
|The Komarov volcanic complex is seen in the foreground in this view from the north toward the southern part of the Gamchen volcanic range. The youngest cone of the Komarov complex, 2070-m-high Komarov, was built at the western end of a 2.5 x 4 km caldera. It is capped by two craters, one at the summit and the other on the upper east flank. The Gamchen massif beyond Komarov consists of three Late-Pleistocene and one Holocene cones. The perfect cone of Kronotsky volcano is seen on the far right horizon.
Copyrighted photo by Philippe Bourseiller (Holocene Kamchataka volcanoes; http://www.kscnet.ru/ivs/volcanoes/holocene/main/main.htm).
|Hydrothermally altered rocks form the summit ridge of Komarov volcano (also known as Komarova) in this view from the east. Komarov is a complex structure situated in the northern half of the Gamchen ridge and lies at the western end of a 2.5 x 4 km caldera. Lengthy Holocene lava flows, such as the one in the foreground, extend beyond the caldera to the east and west. Although no historical eruptions are known from Komarov, growth of the young volcano began only about 1500 years ago.
Copyrighted photo by Vera Ponomareva (Holocene Kamchataka volcanoes; http://www.kscnet.ru/ivs/volcanoes/holocene/main/main.htm).
The following references have all been used during the compilation of data for this volcano, it is not a comprehensive bibliography. 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.
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.
|Large Eruptions of Komarov||Information about large Quaternary eruptions (VEI >= 4) is cataloged in the Large Magnitude Explosive Volcanic Eruptions (LaMEVE) database of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).|
|WOVOdat||WOVOdat is a database of volcanic unrest; instrumentally and visually recorded changes in seismicity, ground deformation, gas emission, and other parameters from their normal baselines. It is sponsored by the World Organization of Volcano Observatories (WOVO) and presently hosted at the Earth Observatory of Singapore.|
|EarthChem||EarthChem develops and maintains databases, software, and services that support the preservation, discovery, access and analysis of geochemical data, and facilitate their integration with the broad array of other available earth science parameters. EarthChem is operated by a joint team of disciplinary scientists, data scientists, data managers and information technology developers who are part of the NSF-funded data facility Integrated Earth Data Applications (IEDA). IEDA is a collaborative effort of EarthChem and the Marine Geoscience Data System (MGDS).|
|Smithsonian Collections||Search the Smithsonian's NMNH Department of Mineral Sciences collections database. Go to the "Search Rocks and Ores" tab and use the Volcano Name drop-down to find samples.|