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Russia · Stratovulcano

Košelev

Koshelev

Tipo
Stratovulcano
Altitudine
1822 m
Ultima eruzione
1690
Koshelev (upper right) is one of the southernmost active volcanoes on the Kamchatka Peninsula, seen here SW of the Kurile Lake caldera. It contains four main cones constructed along an E-W line over a Pleistocene edifice with the central and highest peak being the youngest. An explosive eruption occurred at the end of the 17th century. Alaid, the northernmost volcano of the Kuril Islands, is the peak on the left horizon.
Koshelev (upper right) is one of the southernmost active volcanoes on the Kamchatka Peninsula, seen here SW of the Kurile Lake caldera. It contains four main cones constructed along an E-W line over a Pleistocene edifice with the central and highest peak being the youngest. An explosive eruption occurred at the end of the 17th century. Alaid, the northernmost volcano of the Kuril Islands, is the peak on the left horizon. · Foto: Photo by Nikolai Smelov, 1996 (courtesy of Vera Ponomareva, Inst. Volcanic Geology & Geochemistry, Petropavlovsk).
Tipo
Stratovulcano
Paese
Russia
Regione
Pacifico nord-occidentale / Kuril Volcanic Arc
Altitudine
1822 m
Coordinate
51.356, 156.753
Ultima eruzione
1690
Contesto tettonico
Zona di subduzione / Crosta continentale (> 25 km)
Forma vulcanica
Composito
Roccia principale
Basalto / Picrobasalto
Sintesi geologica

Koshelev is at the southern end of the Kamchatka Peninsula, SW of the Pauzhetka volcano-tectonic depression and NW of Kambalny volcano. It is a complex group of four stratovolcanoes constructed along an E-W line over a Pleistocene shield volcano. Central Koshelev stratovolcano, the highest peak of the volcanic massif, is Holocene in age; N- and SE-flank craters have also been active during the Holocene. Gorely, a Holocene cinder cone related to regional basaltic monogenetic volcanism, is located about 12 km NW. The largest Holocene eruption took place from the eastern cone about 6,500 years ago. An explosive eruption was reported at the end of the 17th century. Major thermal fields are located in the summit crater of Valentin volcano and on the western flanks of west Koshelev volcano.

Storia delle eruzioni

5 registrateGlossario
Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni · Usa le frecce per spostarti tra le barre, Invio per aprire
4550 a.C.~4340 a.C. · 1 eruzioni · VEI max. ?4131 a.C.~3921 a.C. · 1 eruzioni · VEI max. ?1404 a.C.~1195 a.C. · 1 eruzioni · VEI max. ?1531~1741 · 2 eruzioni · VEI max. 34550 a.C.3082 a.C.1404 a.C.631531

Cronologia dettagliata

  1. 1741VEI ?Metodo non indicato
    1741 – fine sconosciuta
  2. 1690 (±10 anni)VEI 3Osservata
    1690 – fine sconosciuta
    SE flank
  3. 1350 a.C.VEI ?Stima geologica
    1350 a.C. – fine sconosciuta
    Northern flank
  4. 4050 a.C.VEI ?Stima geologica
    4050 a.C. – fine sconosciuta
    NW flank (Gorely)
  5. 4550 a.C.VEI ?Stima geologica
    4550 a.C. – fine sconosciuta
    Eastern cone

Vulcani nelle vicinanze

Link esterni

⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.