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Ushishir

Ushishur

Caldera · Russia · 357m

The 1.6-km-wide caldera of Ushishur volcano opens towards the south and formed during an eruption about 9,400 years ago. Two post-caldera lava domes that erupted sometime after a 1769 visit of Captain Snow form islands in the caldera bay. Two older domes in front of the islands are joined by a sand bar to the SE caldera wall. A northern island (top) consists of a portion of the flanks.
The 1.6-km-wide caldera of Ushishur volcano opens towards the south and formed during an eruption about 9,400 years ago. Two post-caldera lava domes that erupted sometime after a 1769 visit of Captain Snow form islands in the caldera bay. Two older domes in front of the islands are joined by a sand bar to the SE caldera wall. A northern island (top) consists of a portion of the flanks. · Photo: Photo by R. Bulgakov, 1990 (Institute of Marine Geology and Geophysics, Yuzhno-Sakhalin). · Wikimedia Commons
Type
Caldera
Country
Russia
Region
Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
Elevation
357m
Coordinates
47.513, 152.814
Last eruption
1884
Tectonic setting
Subduction zone / Oceanic crust (< 15 km)
Landform
Caldera
Major rock type
Andesite / Basaltic Andesite
Geological summary

The subaerial portion of Ushishur volcano in the central Kuriles is exposed in two small islands, the southern containing the summit caldera and the northern a portion of the volcano's flanks. A small 1.6-km-wide caldera that formed about 9,400 years ago is narrowly breached on the south, allowing seawater to fill the caldera. Two andesitic lava domes occupy part of the caldera bay; two other older domes are joined by a sand bar to the SE caldera wall. The two younger domes, erupted sometime after the 1769 visit of Captain Snow, form islands in the bay. A cluster of strong fumaroles and hot springs are present along the SE caldera shoreline, and vigorous submarine hydrothermal activity has modified the geochemistry of water within the caldera bay. Aside from growth of the two younger lava domes, only minor phreatic eruptions have been recorded.

From Wikipedia

Ushishir is a collective name for two uninhabited volcanic islands and several reefs, all being parts of an eponymous partially submerged volcano, 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 "hot spring".

Wikipedia · CC BY-SA · Read full article

Eruption history

Summary (VEI over time)
Click a bar to see individual eruptions
7450 BCE~7139 BCE · 1 eruptions · max VEI 41573~1884 · 3 eruptions · max VEI 17450 BCE5272 BCE2783 BCE605 BCE1573

Detailed timeline

  1. 1884VEI 1Observed
    1884-07 – Ongoing
    SE caldera wall
  2. 1769VEI ?Observed
    1769 – Ongoing
    Center of caldera bay
  3. 1710 (±10 yrs)VEI 1Observed
    1710 – Ongoing
    SE caldera wall
  4. 7450 BCE (±50 yrs)VEI 4Geological estimate
    BCE 7450 – Ongoing

External links

⚠ For reference only. Not for emergency response.