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Ushkovsky

Gunung api majemuk · Russia · 3943 m

Ushkovsky is a large compound volcanic massif located at the NW end of the Klyuchevskaya volcano group. Seen here from the NW, it consists of the flat-topped Ushkovsky (far right), which is capped by an ice-filled 4.5 x 5.5 km caldera, and the adjacent higher Krestovsky peak (center). Numerous scoria cones have formed on its flanks.
Ushkovsky is a large compound volcanic massif located at the NW end of the Klyuchevskaya volcano group. Seen here from the NW, it consists of the flat-topped Ushkovsky (far right), which is capped by an ice-filled 4.5 x 5.5 km caldera, and the adjacent higher Krestovsky peak (center). Numerous scoria cones have formed on its flanks. · Foto: Photo by E.Y. Zhdanova (courtesy of Oleg Volynets, Institute of Volcanology, Petropavlovsk). · Wikimedia Commons
Tipe
Gunung api majemuk
Negara
Russia
Wilayah
Northwestern Pacific Volcanic Regions / Eastern Kamchatka Volcanic Arc
Ketinggian
3943 m
Koordinat
56.113, 160.509
Letusan terakhir
1890
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Composite
Batuan utama
Basalt / Picro-Basalt
Ringkasan geologi

The Ushkovsky (formerly known as Plosky) complex is a large compound volcanic massif located at the NW end of the Kliuchevskaya volcano group. The summit of Krestovsky (Blizhny Plosky) volcano, about 10 km NW of Kliuchevskoy, is the high point of the complex. Linear zones of cinder cones are found on the SW and NE flanks and on lowlands to the west. The Ushkovsky (Daljny Plosky) edifice SE of Krestkovsky is capped by an ice-filled 4.5 x 5.5 km caldera containing two glacier-clad cinder cones with large summit craters. A younger caldera at the summit of Daljny was formed in association with the eruption of large lava flows and pyroclastic material from the Lavovy Shish cinder cones at the foot of the volcano about 8,600 years ago. An explosive eruption took place from the summit cone in 1890.

Ringkasan Wikipedia

Ringkasan Inggris

Ushkovsky is a large volcanic massif located in the central part of the Kamchatka Peninsula, Russia. It is located at the northwestern end of the Klyuchevskaya Sopka volcano group. These volcanoes are also set in a chain linked formation. The highest peak of this massif is Krestovsky. Krestovsky is a stratovolcano, Ushkovsky is a shield volcano.

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Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
7550 BCE~7235 BCE · 1 letusan · VEI maks. ?6921 BCE~6606 BCE · 1 letusan · VEI maks. ?1575~1890 · 1 letusan · VEI maks. 27550 BCE5347 BCE2830 BCE627 BCE1575

Garis waktu rinci

  1. 1890VEI 2Teramati
    1890-04 – Berlangsung
  2. 6670 SM (±150 tahun)VEI ?Perkiraan geologi
    BCE 6670 – Berlangsung
    Lavovy Shish cone group & summit caldera
  3. 7550 SMVEI ?Perkiraan geologi
    BCE 7550 – Berlangsung

Tautan eksternal

⚠ Untuk referensi saja. Bukan untuk tanggap darurat.