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Kikhpinych

Estratovolcán · Russia · 1515 m

Three Holocene cones of Kikhpinych are seen in this view from the west with the Pacific Ocean in the background. The distinct brown feature in the center is the Krab lava dome that grew on the E flank of Savich (back center), the youngest cone of the complex at about 1,400 years old. The peak at right is the mid-Holocene Zapadny cone. In the foreground is the Duga cone, which erupted about 3,200 years ago and produced lava flows up to 10 km long.
Three Holocene cones of Kikhpinych are seen in this view from the west with the Pacific Ocean in the background. The distinct brown feature in the center is the Krab lava dome that grew on the E flank of Savich (back center), the youngest cone of the complex at about 1,400 years old. The peak at right is the mid-Holocene Zapadny cone. In the foreground is the Duga cone, which erupted about 3,200 years ago and produced lava flows up to 10 km long. · Foto: Copyrighted photo by Vera Ponomareva (Holocene Kamchataka volcanoes; http://www.kscnet.ru/ivs/volcanoes/holocene/main/main.htm). · Wikimedia Commons
Tipo
Estratovolcán
País
Russia
Región
Northwestern Pacific Volcanic Regions / Eastern Kamchatka Volcanic Arc
Altitud
1515 m
Coordenadas
54.489, 160.251
Última erupción
1550
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Composite
Roca principal
Basalt / Picro-Basalt
Resumen geológico

Kikhpinych, the youngest stratovolcano of the Eastern Volcanic Zone of Kamchatka, contains three summits constructed along a roughly E-W line above the eroded Pleistocene Pik volcano, NE of the Uzon caldera. Growth of the modern volcano began during the mid-Holocene about 4,800 years ago with construction of the Zapadny cone. After a long quiescence, the younger Savich cone was built about 1,400 years ago, which included strong explosive activity that destroyed part of the Zapadny and Pik cones. Numerous young lava flows mantle the flanks of Savich; it was last active about 400 years ago, when the Krab lava dome grew on its E flank. Numerous thermal fields are found throughout the complex, including two geysers (now the site of vigorous fumaroles) that were active in the summit crater of Stary Kikhpinych prior to burial by a rockfall avalanche that occurred sometime between September 1981 and July 1982.

Resumen de Wikipedia

Resumen en inglés

Kikhpinych is a stratovolcano located in the eastern part of the Kamchatka Peninsula, which feeds the famous Valley of Geysers.

Wikipedia · CC BY-SA · Leer artículo completo

Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
2850 BCE~2650 BCE · 2 erupciones · VEI máx. 4550~750 · 2 erupciones · VEI máx. 3750~950 · 2 erupciones · VEI máx. 31350~1550 · 2 erupciones · VEI máx. 42850 BCE1850 BCE650 BCE3501350

Línea de tiempo detallada

  1. 1550VEI ?Estimación geológica
    1550 – En curso
    East flank of Savich (Krab cone)
  2. 1350VEI 4Estimación geológica
    1350 – En curso
    Savich cone and north flank
  3. 900 (±50 años)VEI 3Estimación geológica
    900 – En curso
    Savich cone
  4. 830 (±25 años)VEI ?Estimación geológica
    830 – En curso
    Savich cone
  5. 650VEI ?Estimación geológica
    650 – En curso
    Savich cone
  6. 550VEI 3Estimación geológica
    550 – En curso
    East side of Zapadny, Savich cone
  7. 2780 a. C. (±25 años)VEI 4Estimación geológica
    BCE 2780 – En curso
    Zapadny
  8. 2850 a. C.VEI 3Estimación geológica
    BCE 2850 – En curso
    Zapadny

Enlaces externos

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