Ushkovsky
Gunung api majemuk · Russia · 3943 m

- 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 InggrisUshkovsky 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
Garis waktu rinci
- 1890VEI 2Teramati1890-04 – Berlangsung
- 6670 SM (±150 tahun)VEI ?Perkiraan geologiBCE 6670 – BerlangsungLavovy Shish cone group & summit caldera
- 7550 SMVEI ?Perkiraan geologiBCE 7550 – Berlangsung
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.