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Zhupanovsky

Volcán compuesto · Russia · 2899 m

All four cones forming the WNW-trending Zhupanovsky massif are seen in this view from the west. The upper peak forms the summit of the complex. Steam plumes rise from the historically active crater in the center of the only Holocene cone; known eruptions have consisted of relatively minor explosions.
All four cones forming the WNW-trending Zhupanovsky massif are seen in this view from the west. The upper peak forms the summit of the complex. Steam plumes rise from the historically active crater in the center of the only Holocene cone; known eruptions have consisted of relatively minor explosions. · Foto: Photo by Oleg Volynets (Institute of Volcanology, Petropavlovsk). · Wikimedia Commons
Tipo
Volcán compuesto
País
Russia
Región
Northwestern Pacific Volcanic Regions / Eastern Kamchatka Volcanic Arc
Altitud
2899 m
Coordenadas
53.589, 159.150
Última erupción
2016
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Composite
Roca principal
Andesite / Basaltic Andesite
Resumen geológico

The Zhupanovsky volcanic massif consists of four overlapping stratovolcanoes along a WNW-trending ridge. The elongated complex was constructed within a Pliocene-early Pleistocene caldera whose rim is exposed only on the eastern side. Three of the stratovolcanoes were built during the Pleistocene. An early Holocene stage of frequent moderate and weak eruptions from 7,000 to 5,000 years before present (BP) was followed by a period of infrequent larger eruptions that produced pyroclastic flows. The last major eruption took place about 800-900 BP. Recorded eruptions have consisted of relatively minor explosions from Priemysh, the third cone from the E about 2.5 km from the summit peak.

Resumen de Wikipedia

Resumen en inglés

Zhupanovsky is a volcanic massif located in the southeastern part of the Kamchatka Peninsula, Russia. It consists of four overlapping stratovolcanoes. After 54 years of inactivity, the volcano began erupting on 23 October 2013 and again in 2014, continuing nonstop into 2016.

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Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
5050 BCE~4814 BCE · 1 erupciones · VEI máx. ?3166 BCE~2930 BCE · 1 erupciones · VEI máx. ?339 BCE~104 BCE · 1 erupciones · VEI máx. ?104 BCE~132 · 1 erupciones · VEI máx. ?838~1074 · 1 erupciones · VEI máx. ?1545~1780 · 1 erupciones · VEI máx. 21780~2016 · 10 erupciones · VEI máx. 35050 BCE3401 BCE1517 BCE1321780

Línea de tiempo detallada

  1. 2016VEI 2Observado
    2016-11-20 – 2016-11-20
    Priemysh Crater
  2. 2015VEI 3Observado
    2015-11-28 – 2016-03-25
    Priemysh Crater
  3. 2014VEI 3Observado
    2014-06-06 – 2015-08-06
    Priemysh Crater
  4. 2013VEI 2Observado
    2013-10-23 – 2013-10-26
    Summit crater
  5. 1959VEI 2Observado
    1959-07-02 – En curso
  6. 1956VEI 2Observado
    1956-12-27 – 1957-06-16
    Middle crater, east crater
  7. 1940VEI 2Observado
    1940-01 – 1940-02
  8. 1929VEI 2Observado
    1929 – En curso
  9. 1925VEI 2Observado
    1925 – En curso
  10. 1882VEI 2Observado
    1882 – En curso
  11. 1776VEI 2Observado
    1776-10 – En curso
  12. 1000 (±500 años)VEI ?Estimación geológica
    1000 – En curso
  13. 50 a. C.VEI ?Estimación geológica
    BCE 50 – En curso
  14. 220 a. C. (±50 años)VEI ?Estimación geológica
    BCE 220 – En curso
  15. 3050 a. C.VEI ?Estimación geológica
    BCE 3050 – En curso
  16. 5050 a. C.VEI ?Estimación geológica
    BCE 5050 – En curso

Enlaces externos

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