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The Global Volcanism Program has no activity reports for Otdelniy.
The Global Volcanism Program has no Weekly Reports available for Otdelniy.
The Global Volcanism Program has no Bulletin Reports available for Otdelniy.
The early Holocene Otdelniy shield volcano (Masurenkov, 1980) lies east of the Savan River, across from the Pleistocene Savan volcano. The 719-m-high Otdelniy lies at the west end of a large group of late-Pleistocene to Holocene pyroclastic cones. It, along with Tundroviy and adjacent unnamed shield volcanoes, is adjacent to a large group of late-Pleistocene to Holocene basaltic pyroclastic cones located about halfway between Khodutka and Opala volcanoes. The cones and associated lava fields are located at the headwaters of the Savan and Asacha rivers, which drain to the Sea of Okhotsk and the Pacific Ocean, respectively. Three groups of late-Pleistocene to Holocene pyroclastic cones and associated lava fields are also located along a roughly 20-km-wide area between the Opala and Savan rivers, SE, south, and SW of massive Opala volcano.
The Global Volcanism Program is not aware of any Holocene eruptions from Otdelniy. If this volcano has had large eruptions (VEI >= 4) prior to 10,000 years ago, information might be found on the Otdelniy 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|
|Tundroviy||Shield volcano||739 m||52° 15' 0" N||157° 36' 0" E|
|A large group of small shield volcanoes and pyroclastic cones lies at the bottom center of this NASA Space Shuttle image (with north to the top). Otdelniy, Tundroviy and other adjacent unnamed shield volcanoes are surrounded by a large group of late-Pleistocene to Holocene pyroclastic cones SE of Opala (the conical stratovolcano at the upper left) and SW of Asacha volcano (right-center). Scattered groups of young pyroclastic cones are also located south of Opala caldera, whose rim is seen at the left-center.
NASA Space Shuttle image ISS006-E-36667, 2003 (http://eol.jsc.nasa.gov/).
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).