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Barkhatnaya

Barkhatnaya Sopka

Campo vulcanico · Russia · 874 m

The Holocene scoria cones of Barkhatnaya Sopka are located on a plateau 13 km N of Vilyuchik volcano on an uplifted eroded Miocene-Pliocene block. In this view looking NE, the Mt. Barkhatnaya cone which formed 3,000-4,000 years ago is to the left, and the reddish hill to the right is an early Holocene scoria cone. The white hill in the center is a part of an eroded rhyolitic body.
The Holocene scoria cones of Barkhatnaya Sopka are located on a plateau 13 km N of Vilyuchik volcano on an uplifted eroded Miocene-Pliocene block. In this view looking NE, the Mt. Barkhatnaya cone which formed 3,000-4,000 years ago is to the left, and the reddish hill to the right is an early Holocene scoria cone. The white hill in the center is a part of an eroded rhyolitic body. · Foto: Coyrighted photo by Oleg Dirksen (Holocene Kamchataka volcanoes; http://www.kscnet.ru/ivs/volcanoes/holocene/main/main.htm).
Tipo
Campo vulcanico
Paese
Russia
Regione
Pacifico nord-occidentale / Kuril Volcanic Arc
Altitudine
874 m
Coordinate
52.802, 158.240
Ultima eruzione
-3550
Contesto tettonico
Subduction zone / Continental crust (> 25 km)
Forma vulcanica
Cluster
Roccia principale
Basalt / Picro-Basalt
Sintesi geologica

The Barkhatnaya Sopka group of Pleistocene andesitic-to-rhyolitic lava domes and Holocene basaltic pyroclastic cones is located along the Paratunka River about 30 km NNW of Gorely volcano. The cinder cones are sitting on an uplifted block of eroded Miocene-Pliocene rocks. Most of the younger cones lie on the S and SE sides of the volcanic field. The Barkhatnaya cinder cone formed about 3,000-4,000 years ago (Ponomareva, 1992 p.c.).

Storia delle eruzioni

Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni
3550 BCE~3550 BCE · 1 eruzioni · VEI max. ?3550 BCE3550 BCE3549 BCE3549 BCE3549 BCE

Cronologia dettagliata

  1. 3550 a.C.VEI ?Stima geologica
    BCE 3550 – In corso

Link esterni

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