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Rusia · Stratovolkan

Komarov

Tipe
Stratovolkan
Ketinggian
2065 m
Letusan terakhir
950
Hydrothermally altered rocks form the summit ridge of Komarov in this view from the east. Komarov is a complex structure in the northern half of the Gamchen ridge and lies at the western end of a 2.5 x 4 km caldera. Holocene lava flows, such as the one in the foreground, extend beyond the caldera to the east and west.
Hydrothermally altered rocks form the summit ridge of Komarov in this view from the east. Komarov is a complex structure in the northern half of the Gamchen ridge and lies at the western end of a 2.5 x 4 km caldera. Holocene lava flows, such as the one in the foreground, extend beyond the caldera to the east and west. · Foto: Copyrighted photo by Vera Ponomareva (Holocene Kamchataka volcanoes; http://www.kscnet.ru/ivs/volcanoes/holocene/main/main.htm).
Tipe
Stratovolkan
Negara
Rusia
Wilayah
Pasifik Barat Laut / Eastern Kamchatka Volcanic Arc
Ketinggian
2065 m
Koordinat
55.033, 160.725
Letusan terakhir
950
Kondisi tektonik
Zona subduksi / Kerak benua (> 25 km)
Bentuk lahan
Komposit
Batuan utama
Basal / Pikrobasal
Ringkasan geologi

Komarov volcano is a complex structure along the Gamchen ridge. The summit area includes two irregular craters ~300m in diameter. Lengthy Holocene lava flows extend to the east and west. Growth began about 1,500 years ago following cessation of activity at Vysoky volcano. No reported eruptions are known, but the summit region has undergone extensive hydrothermal alteration, and fumarolic areas occur there and on the northern and southern flanks.

Ringkasan Wikipedia

Ringkasan Inggris

Komarov is an inactive stratovolcano located in the southeastern part of the Kamchatka Peninsula, Russia. It was named after Vladimir L. Komarov.

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Riwayat letusan

2 tercatatGlosarium
Ringkasan (VEI dari waktu ke waktu)
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450~500 · 1 letusan · VEI maks. 0900~950 · 1 letusan · VEI maks. ?450550700800900

Garis waktu rinci

  1. 950VEI ?Perkiraan geologi
    950 – akhir tidak diketahui
  2. 450VEI 0Perkiraan geologi
    450 – akhir tidak diketahui

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