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Barkhatnaya

Barkhatnaya Sopka

Tipe
Medan gunung api
Ketinggian
874 m
Letusan terakhir
-3550
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).
Tipe
Medan gunung api
Negara
Rusia
Wilayah
Pasifik Barat Laut / Kuril Volcanic Arc
Ketinggian
874 m
Koordinat
52.802, 158.240
Letusan terakhir
-3550
Kondisi tektonik
Zona subduksi / Kerak benua (> 25 km)
Bentuk lahan
Gugusan gunung api
Batuan utama
Basal / Pikrobasal

Ringkasan geologi

Teks asli bahasa Inggris

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.

Kutipan dari Global Volcanism Program, Smithsonian Institution · Baca ringkasan lengkap di GVP →

Ringkasan Wikipedia

Ringkasan Inggris

Barkhatnaya Sopka is a volcano located in the southern part of Kamchatka Peninsula, Russia, along the Paratunka River.

Wikipedia · CC BY-SA · Lanjutkan membaca di Wikipedia bahasa Inggris →

Riwayat letusan

1 tercatatGlosarium

Ringkasan catatan

Letusan terkonfirmasi
1
Letusan tidak pasti
0
Rentang catatan terkonfirmasi
3550 SM – 3550 SM
Letusan terkonfirmasi terbesar
Tidak ada VEI tercatat
Letusan terkonfirmasi sejak 1900
0
Ringkasan (VEI dari waktu ke waktu)
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3550 SM~3550 SM · 1 letusan · VEI maks. ?3550 SM3550 SM3549 SM3549 SM3549 SM

Garis waktu rinci

  1. 3550 SMVEI ?Perkiraan geologi
    3550 SM – akhir tidak diketahui

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