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The Global Volcanism Program has no activity reports for Ostanets.
The Global Volcanism Program has no Weekly Reports available for Ostanets.
The Global Volcanism Program has no Bulletin Reports available for Ostanets.
The Holocene Ostanets shield volcano (Masurenkov, 1980), located south of the Pleistocene Savan volcano, is surrounded by a large group of late-Pleistocene to Holocene cinder cones. Small pyroclastic cone groups also occur north and east of Igolki volcano, which is located about 30 km SW of Savan volcano.
The Global Volcanism Program is not aware of any Holocene eruptions from Ostanets. If this volcano has had large eruptions (VEI >= 4) prior to 10,000 years ago, information might be found on the Ostanets page in the LaMEVE (Large Magnitude Explosive Volcanic Eruptions) database, a part of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).
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.
|Feature Name||Feature Type||Elevation||Latitude||Longitude|
|Khetik||Shield volcano||925 m||52° 6' 0" N||157° 15' 0" E|
The Global Volcanism Program has no photographs available for Ostanets.
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.
Erlich E N, 1985. . (pers. comm.).
Fedotov S A, Masurenkov Y P (eds), 1991. Active Volcanoes of Kamchatka. Moscow: Nauka Pub, 2 volumes.
Masurenkov Y P (ed), 1980. Volcanic Center: Structure, Dynamics and Products. Moscow: Nauka Pub, 299 p (in Russian).