- Info & Contacts
The Global Volcanism Program has no activity reports for Kekurny.
The Global Volcanism Program has no Weekly Reports available for Kekurny.
The Global Volcanism Program has no Bulletin Reports available for Kekurny.
Kekurny is the northernmost of two overlapping small late-Quaternary Icelandic-type basaltic to basaltic-andesite shield volcanoes located north of Anaun volcano and west of Krainy volcano in the southern Sredinny Range. A chain of small cinder cones was constructed along a NE-SW-trending rift cutting across the 1377-m-high volcano. The 1336-m-high Bunanya shield volcano is located immediately to the south of Kekurny and has cinder cones on its NE flank. Early geologic studies in the Sredinny Range (Ogorodov et al., 1972) identified numerous Holocene eruptive centers based primarily on morphological criteria. However, later work has suggested that Sredinny Range volcanoes are less mantled by Holocene tephras than eastern Kamchatka volcanoes and therefore appear more youthful, so that Holocene eruptions are uncertain for many of these Sredinny Range eruptive vents.
The Global Volcanism Program is not aware of any Holocene eruptions from Kekurny. If this volcano has had large eruptions (VEI >= 4) prior to 10,000 years ago, information might be found on the Kekurny 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|
|Bunanya||Shield volcano||1336 m||56° 22' 0" N||158° 52' 0" E|
The Global Volcanism Program has no photographs available for Kekurny.
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.).
Erlich E N, Gorshkov G S (eds), 1979. Quaternary volcanism and tectonics in Kamchatka. Bull Volc, 42:1-4.
IAVCEI, 1973-80. Post-Miocene Volcanoes of the World. IAVCEI Data Sheets, Rome: Internatl Assoc Volc Chemistry Earth's Interior..
Ogorodov N V, Kozhemyaka N N, Vazheevskaya A A, Ogorodov A S, 1972. Volcanoes and the Quaternary Volcanism of the Sredinny Ridge in Kamchatka. Moscow: Nauka Pub, 190 p (in Russian).
Ponomareva V V, 2001. . (pers. comm.).