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Čirinkotan

Chirinkotan

Stratovulcano · Russia · 724 m

The 3-km-wide island of Chirinkotan is the emergent summit of a volcano that rises 3 km from the floor of the Kuril Basin. It lies at the far end of an E-W-trending volcanic chain that extends nearly 50 km W of the central part of the main Kuril Islands arc. Historical eruptions have been recorded here since the 18th century, including one observed by Captain Snow.
The 3-km-wide island of Chirinkotan is the emergent summit of a volcano that rises 3 km from the floor of the Kuril Basin. It lies at the far end of an E-W-trending volcanic chain that extends nearly 50 km W of the central part of the main Kuril Islands arc. Historical eruptions have been recorded here since the 18th century, including one observed by Captain Snow. · Foto: Photo by R. Bulgakov, 1990 (Institute of Marine Geology and Geophysics, Yuzhno-Sakhalin). · Wikimedia Commons
Tipo
Stratovulcano
Paese
Russia
Regione
Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
Altitudine
724 m
Coordinate
48.980, 153.480
Ultima eruzione
2022
Contesto tettonico
Subduction zone / Intermediate crust (15-25 km)
Forma vulcanica
Composite
Roccia principale
Andesite / Basaltic Andesite
Sintesi geologica

The small, mostly unvegetated 3-km-wide island of Chirinkotan occupies the far end of an E-W volcanic chain that extends nearly 50 km W of the central part of the main Kuril Islands arc. It is the emergent summit of a volcano that rises 3000 m from the floor of the Kuril Basin. A small 1-km-wide caldera about 300-400 m deep is open to the SW. Lava flows from a cone within the breached crater reached the shore of the island. Historical eruptions have been recorded since the 18th century. Lava flows were observed by the English fur trader Captain Snow in the 1880s.

Sintesi da Wikipedia

Čirinkotan è un'isola russa che fa parte dell'arcipelago delle Isole Curili ed è situata nel Mare di Ochotsk. Amministrativamente fa parte del Severo-Kuril'skij rajon dell'oblast' di Sachalin, nel Circondario federale dell'Estremo Oriente. Il suo nome viene dalla lingua ainu e significa "valanga di fango". L'isola è disabitata.

Wikipedia · CC BY-SA · Leggi l'articolo completo →

Storia delle eruzioni

Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni
1760~1786 · 1 eruzioni · VEI max. 21865~1891 · 1 eruzioni · VEI max. 01891~1917 · 1 eruzioni · VEI max. ?1943~1970 · 1 eruzioni · VEI max. 21970~1996 · 2 eruzioni · VEI max. 21996~2022 · 6 eruzioni · VEI max. 317601812189119431996

Cronologia dettagliata

  1. 2022VEI 2Osservata
    2022-10-07 – 2022-10-07
  2. 2021VEI 2Osservata
    2021-08-08 – 2021-08-26
  3. 2016VEI 3Osservata
    2016-11-29 – 2017-04-07
    Summit crater
  4. 2014VEI 2Osservata
    2014-11-21 – 2015-08-10
    Summit crater
  5. 2013VEI 1Osservata
    2013-06-11 – 2014-06-01
    Summit crater
  6. 2004VEI 2Osservata
    2004-07-20 – 2004-07-20
  7. 1986VEI 1Osservata
    1986-10-11 – 1986-10-12
  8. 1979VEI 2Osservata
    1979-04-16 – 1980-10-10
  9. 1955VEI 2Osservata
    1955-07-02 – In corso
    Floor of summit explosion crater
  10. 1900 (±10 anni)VEI ?Osservata
    1900 – In corso
  11. 1884 (±6 anni)VEI 0Osservata
    1884 – In corso
    North foot of inner summit cone
  12. 1760VEI 2Stima geologica
    1760 – In corso

Link esterni

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