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Chirinkotan

Estratovolcán · 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
Estratovolcán
País
Russia
Región
Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
Altitud
724 m
Coordenadas
48.980, 153.480
Última erupción
2022
Contexto tectónico
Subduction zone / Intermediate crust (15-25 km)
Forma volcánica
Composite
Roca principal
Andesite / Basaltic Andesite
Resumen geológico

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.

Resumen de Wikipedia

Chirinkotan es una isla rusa en el archipiélago de las Kuriles. Tiene una superficie de 6 km². Pertenece al grupo de las Kuriles septentrionales.

Wikipedia · CC BY-SA · Leer artículo completo →

Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
1760~1786 · 1 erupciones · VEI máx. 21865~1891 · 1 erupciones · VEI máx. 01891~1917 · 1 erupciones · VEI máx. ?1943~1970 · 1 erupciones · VEI máx. 21970~1996 · 2 erupciones · VEI máx. 21996~2022 · 6 erupciones · VEI máx. 317601812189119431996

Línea de tiempo detallada

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

Enlaces externos

⚠ Solo como referencia. No apto para respuesta ante emergencias.