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Kostakan

Cono piroclástico · Russia · 1150 m

A N-S-trending chain of scoria cones lies in the Kostakan valley south of Bakening volcano. The 600-year-old Glavny scoria cone (left center) is surrounded by its lava flow, which dammed a small river to form beautiful Kostakan lake. Two small vegetated early Holocene cones lie along the opposite side of the lake.
A N-S-trending chain of scoria cones lies in the Kostakan valley south of Bakening volcano. The 600-year-old Glavny scoria cone (left center) is surrounded by its lava flow, which dammed a small river to form beautiful Kostakan lake. Two small vegetated early Holocene cones lie along the opposite side of the lake. · Foto: Copyrighted photo by Sergei Konyaev (Holocene Kamchataka volcanoes; http://www.kscnet.ru/ivs/volcanoes/holocene/main/main.htm).
Tipo
Cono piroclástico
País
Russia
Región
Northwestern Pacific Volcanic Regions / Eastern Kamchatka Volcanic Arc
Altitud
1150 m
Coordenadas
53.833, 158.052
Última erupción
1350
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Minor (Basaltic)
Roca principal
Basalt / Picro-Basalt
Resumen geológico

A group of basaltic cinder cones lies south of Bakening volcano, west of the Srednaya Avacha (Middle Avacha) river valley. They are part of a broad zone of regional late Pleistocene to Holocene basaltic volcanism west of the Eastern volcanic zone of Kamchatka that extends from the Kostakan Lake area to the south. Several of the cinder cones are breached by lava flows, some of which extend into the Srednaya Avacha valley. The highest-elevation vent, Zmeya crater, was constructed within a landslide scarp. An unnamed maar is located about 2 km S of Kostakan Lake. Eruptions have occurred during two time periods, between about 11,000 to 7,000 years ago and between about 1,200 and 600 years ago.

Resumen de Wikipedia

Resumen en inglés

Kostakan is a north-south trending chain of cinder cones located in the southern part of the Kamchatka Peninsula, Russia.

Wikipedia · CC BY-SA · Leer artículo completo

Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
8050 BCE~7737 BCE · 1 erupciones · VEI máx. 36797 BCE~6483 BCE · 1 erupciones · VEI máx. 3723~1037 · 2 erupciones · VEI máx. 31037~1350 · 2 erupciones · VEI máx. 28050 BCE5857 BCE3350 BCE1157 BCE1037

Línea de tiempo detallada

  1. 1350VEI 1Estimación geológica
    1350 – En curso
    Glavny
  2. 1200 (±50 años)VEI 2Estimación geológica
    1200 – En curso
    Glavny
  3. 1000 (±50 años)VEI 3Estimación geológica
    1000 – En curso
    Serpovidny
  4. 800 (±50 años)VEI 3Estimación geológica
    800 – En curso
    Maar S of Lake Kostakan, Krasny cone
  5. 6550 a. C. (±500 años)VEI 3Estimación geológica
    BCE 6550 – En curso
    Ochkovy
  6. 8050 a. C. (±1000 años)VEI 3Estimación geológica
    BCE 8050 – En curso
    Domashnii

Enlaces externos

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