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Ketoy

Ketoi

Stratovolcano · Russia · 1172m

The roughly 10-km-wide Ketoi island is shown in this September 2018 Planet Labs satellite image monthly mosaic (N is at the top). Ketoi is the older edifice and caldera, and Pallas Peak is the cone with a summit crater that has formed within it, NE of Ketoi Lake. Fumaroles are active on the NE flank of the cone.
The roughly 10-km-wide Ketoi island is shown in this September 2018 Planet Labs satellite image monthly mosaic (N is at the top). Ketoi is the older edifice and caldera, and Pallas Peak is the cone with a summit crater that has formed within it, NE of Ketoi Lake. Fumaroles are active on the NE flank of the cone. · Photo: Satellite image courtesy of Planet Labs Inc., 2018 (https://www.planet.com/). · Wikimedia Commons
Type
Stratovolcano
Country
Russia
Region
Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
Elevation
1172m
Coordinates
47.350, 152.475
Last eruption
1960
Tectonic setting
Subduction zone / Oceanic crust (< 15 km)
Landform
Composite
Major rock type
Andesite / Basaltic Andesite
Geological summary

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.

From Wikipedia

Ketoy is an uninhabited volcanic island located in the centre of the Kuril Islands chain in the Sea of Okhotsk in the northwest Pacific Ocean. Its name is derived from the Ainu language for "skeleton" or "bad".

Wikipedia · CC BY-SA · Read full article

Eruption history

Summary (VEI over time)
Click a bar to see individual eruptions
1843~1861 · 1 eruptions · max VEI 21913~1931 · 1 eruptions · max VEI 21948~1966 · 1 eruptions · max VEI 22001~2018 · 2 eruptions · max VEI 118431878193119662001

Detailed timeline

  1. 2018VEI 1Observed
    2018-09-21 – 2018-09-21
  2. 2013VEI ?Observed
    2013-07-25 – 2013-08-12
    Pallas Peak
  3. 1960VEI 2Observed
    1960-09-27 – Ongoing
    Pallas Peak
  4. 1924VEI 2Observed
    1924 – Ongoing
    Pallas Peak
  5. 1843VEI 2Observed
    1843-07 – 1846
    Pallas Peak

External links

⚠ For reference only. Not for emergency response.