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Kostakan

Cono piroclastico · 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 piroclastico
Paese
Russia
Regione
Northwestern Pacific Volcanic Regions / Eastern Kamchatka Volcanic Arc
Altitudine
1150 m
Coordinate
53.833, 158.052
Ultima eruzione
1350
Contesto tettonico
Subduction zone / Continental crust (> 25 km)
Forma vulcanica
Minor (Basaltic)
Roccia principale
Basalt / Picro-Basalt
Sintesi geologica

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.

Sintesi da Wikipedia

Riassunto in inglese

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

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Storia delle eruzioni

Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni
8050 BCE~7737 BCE · 1 eruzioni · VEI max. 36797 BCE~6483 BCE · 1 eruzioni · VEI max. 3723~1037 · 2 eruzioni · VEI max. 31037~1350 · 2 eruzioni · VEI max. 28050 BCE5857 BCE3350 BCE1157 BCE1037

Cronologia dettagliata

  1. 1350VEI 1Stima geologica
    1350 – In corso
    Glavny
  2. 1200 (±50 anni)VEI 2Stima geologica
    1200 – In corso
    Glavny
  3. 1000 (±50 anni)VEI 3Stima geologica
    1000 – In corso
    Serpovidny
  4. 800 (±50 anni)VEI 3Stima geologica
    800 – In corso
    Maar S of Lake Kostakan, Krasny cone
  5. 6550 a.C. (±500 anni)VEI 3Stima geologica
    BCE 6550 – In corso
    Ochkovy
  6. 8050 a.C. (±1000 anni)VEI 3Stima geologica
    BCE 8050 – In corso
    Domashnii

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