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Ušišir

Ushishur

Caldera · Russia · 357 m

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. · Foto: Photo by R. Bulgakov, 1990 (Institute of Marine Geology and Geophysics, Yuzhno-Sakhalin). · Wikimedia Commons
Tipo
Caldera
Paese
Russia
Regione
Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
Altitudine
357 m
Coordinate
47.513, 152.814
Ultima eruzione
1884
Contesto tettonico
Subduction zone / Oceanic crust (< 15 km)
Forma vulcanica
Caldera
Roccia principale
Andesite / Basaltic Andesite
Sintesi geologica

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.

Sintesi da Wikipedia

Le isole Ušišir sono due isole russe che fanno parte dell'arcipelago delle Isole Curili e sono situate tra il Mare di Ochotsk e l'Oceano Pacifico settentrionale. Amministrativamente fanno parte del Severo-Kuril'skij rajon dell'oblast' di Sachalin, nel Circondario federale dell'Estremo Oriente. Il loro nome viene dalla lingua ainu e significa "sorgenti termali". Le isole sono disabitate.

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Storia delle eruzioni

Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni
7450 BCE~7139 BCE · 1 eruzioni · VEI max. 41573~1884 · 3 eruzioni · VEI max. 17450 BCE5272 BCE2783 BCE605 BCE1573

Cronologia dettagliata

  1. 1884VEI 1Osservata
    1884-07 – In corso
    SE caldera wall
  2. 1769VEI ?Osservata
    1769 – In corso
    Center of caldera bay
  3. 1710 (±10 anni)VEI 1Osservata
    1710 – In corso
    SE caldera wall
  4. 7450 a.C. (±50 anni)VEI 4Stima geologica
    BCE 7450 – In corso

Link esterni

⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.