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Gamčen

Gamchen

Vulcano complesso · Russia · 2539 m

The Gamchen massif, consisting of one Holocene and three late-Pleistocene cones, is seen here from the SE. The reddish Holocene cone in the foreground is Barany and has a 500-m-wide, 200-m-deep crater. Stratigraphic evidence indicates that it grew during several episodes of activity 3,600-3,000 years ago. Yuzhny Gamchen (center) forms the high point of the massif. Kizimen volcano is seen on the distant horizon left of Gamchen's summit.
The Gamchen massif, consisting of one Holocene and three late-Pleistocene cones, is seen here from the SE. The reddish Holocene cone in the foreground is Barany and has a 500-m-wide, 200-m-deep crater. Stratigraphic evidence indicates that it grew during several episodes of activity 3,600-3,000 years ago. Yuzhny Gamchen (center) forms the high point of the massif. Kizimen volcano is seen on the distant horizon left of Gamchen's summit. · Foto: Copyrighted photo by Philippe Bourseiller (Holocene Kamchataka volcanoes; http://www.kscnet.ru/ivs/volcanoes/holocene/main/main.htm). · Wikimedia Commons
Tipo
Vulcano complesso
Paese
Russia
Regione
Northwestern Pacific Volcanic Regions / Eastern Kamchatka Volcanic Arc
Altitudine
2539 m
Coordinate
54.974, 160.703
Ultima eruzione
-188
Contesto tettonico
Subduction zone / Continental crust (> 25 km)
Forma vulcanica
Composite
Roccia principale
Basalt / Picro-Basalt
Sintesi geologica

Gamchen is a complex volcano composed of four stratovolcanoes, one of which is of Holocene age. Yuzhny Gamchen and Severny Gamchen are steep-sided eroded stratovolcanoes of Pleistocene age. Edifice-collapse events during the early Holocene produced several large debris-avalanche deposits below the eastern flanks. Molodoi, a small stratovolcano with a shallow crater, is located on the E flank of Severvy Gamchen. Barany, a young stratovolcano with a crater 500 m wide and 200 m deep, is located on the SE flank of Yuzhny Gamchen. Barany is the source of a lava field extending to the E and NE that was active between about 3,600 and 3,000 years ago. Lava domes are found on the flanks of the volcanoes; the youngest of these is Lukovitsa dome, which formed during the final stages of activity at Barany. No reported eruptions are known.

Sintesi da Wikipedia

Il Gamčen è un vulcano complesso situato nel sud-est della penisola della Kamčatka, nella Russia orientale, 110 km a sud del vulcano Bezymjannyj. Appartiene al gruppo vulcanico Kizimen-Gamčen, formato da cinque vulcani della Catena Orientale. È situato all'interno della riserva naturale di Kronockij, classificata come Patrimonio dell'umanità dall'UNESCO.

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Storia delle eruzioni

Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni
1650 BCE~1504 BCE · 1 eruzioni · VEI max. ?627 BCE~480 BCE · 1 eruzioni · VEI max. ?334 BCE~188 BCE · 1 eruzioni · VEI max. ?1650 BCE1358 BCE919 BCE627 BCE334 BCE

Cronologia dettagliata

  1. 188 a.C. (±80 anni)VEI ?Stima geologica
    BCE 188 – In corso
  2. 550 a.C.VEI ?Stima geologica
    BCE 550 – In corso
    SE flank (Barany, Lukovitsa)
  3. 1650 a.C.VEI ?Stima geologica
    BCE 1650 – In corso
    SE flank (Barany)

Link esterni

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