Rusia · Gunung api majemuk
Ushkovsky
- Tipe
- Gunung api majemuk
- Ketinggian
- 3943 m
- Letusan terakhir
- 1890

- Tipe
- Gunung api majemuk
- Negara
- Rusia
- Wilayah
- Pasifik Barat Laut / Eastern Kamchatka Volcanic Arc
- Ketinggian
- 3943 m
- Koordinat
- 56.113, 160.509
- Letusan terakhir
- 1890
- Kondisi tektonik
- Zona subduksi / Kerak benua (> 25 km)
- Bentuk lahan
- Komposit
- Batuan utama
- Basal / Pikrobasal
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
3 tercatatGlosariumGaris waktu rinci
- 1890VEI 2Teramati1890-04-16 – akhir tidak diketahui
- 6670 SM (±150 tahun)VEI ?Perkiraan geologi6670 SM – akhir tidak diketahuiLavovy Shish cone group & summit caldera
- 7550 SMVEI ?Perkiraan geologi7550 SM – akhir tidak diketahui
Gunung api terdekat
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.