Ketoy
Ketoi
Stratovolkan · Russia · 1172 m

- Tipe
- Stratovolkan
- Negara
- Russia
- Wilayah
- Pasifik Barat Laut / Kuril Volcanic Arc
- Ketinggian
- 1172 m
- Koordinat
- 47.350, 152.475
- Letusan terakhir
- 1960
- Kondisi tektonik
- Subduction zone / Oceanic crust (< 15 km)
- Bentuk lahan
- Composite
- Batuan utama
- Andesite / Basaltic Andesite
Ringkasan geologi
The circular 10-km-wide Ketoi island, which rises across the 19-km-wide Diana Strait from Simushir Island, hosts of one of the most complex volcanic structures of the Kuril Islands. The rim of a 5-km-wide Pleistocene caldera is exposed only on the NE side. A younger stratovolcano forming the NW part of the island is cut by a horst-and-graben structure containing two solfatara fields. A 1.5-km-wide freshwater lake fills an explosion crater in the center of the island. Pallas Peak, a large andesitic cone in the NE part of the caldera, is truncated by a 550-m-wide crater containing a brilliantly colored turquoise crater lake. Lava flows from Pallas Peak overtop the caldera rim and descend nearly 5 km to the SE coast. The first historical eruption of Pallas Peak, during 1843-46, was its largest.
Riwayat letusan
Garis waktu rinci
- 2018VEI 1Teramati2018-09-21 – 2018-09-21
- 2013VEI ?Teramati2013-07-25 – 2013-08-12Pallas Peak
- 1960VEI 2Teramati1960-09-27 – BerlangsungPallas Peak
- 1924VEI 2Teramati1924-07-02 – BerlangsungPallas Peak
- 1843VEI 2Teramati1843-07-16 – 1846-07-02Pallas Peak
Tautan eksternal
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