Kostakan
Cono piroclastico · Russia · 1150 m

- 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 ingleseKostakan is a north-south trending chain of cinder cones located in the southern part of the Kamchatka Peninsula, Russia.
Wikipedia · CC BY-SA · Leggi l'articolo completo →
Storia delle eruzioni
Cronologia dettagliata
- 1350VEI 1Stima geologica1350 – In corsoGlavny
- 1200 (±50 anni)VEI 2Stima geologica1200 – In corsoGlavny
- 1000 (±50 anni)VEI 3Stima geologica1000 – In corsoSerpovidny
- 800 (±50 anni)VEI 3Stima geologica800 – In corsoMaar S of Lake Kostakan, Krasny cone
- 6550 a.C. (±500 anni)VEI 3Stima geologicaBCE 6550 – In corsoOchkovy
- 8050 a.C. (±1000 anni)VEI 3Stima geologicaBCE 8050 – In corsoDomashnii
Link esterni
⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.