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Komarov

Estratovolcán · Russia · 2065 m

Hydrothermally altered rocks form the summit ridge of Komarov in this view from the east. Komarov is a complex structure in the northern half of the Gamchen ridge and lies at the western end of a 2.5 x 4 km caldera. Holocene lava flows, such as the one in the foreground, extend beyond the caldera to the east and west.
Hydrothermally altered rocks form the summit ridge of Komarov in this view from the east. Komarov is a complex structure in the northern half of the Gamchen ridge and lies at the western end of a 2.5 x 4 km caldera. Holocene lava flows, such as the one in the foreground, extend beyond the caldera to the east and west. · Foto: Copyrighted photo by Vera Ponomareva (Holocene Kamchataka volcanoes; http://www.kscnet.ru/ivs/volcanoes/holocene/main/main.htm).
Tipo
Estratovolcán
País
Russia
Región
Northwestern Pacific Volcanic Regions / Eastern Kamchatka Volcanic Arc
Altitud
2065 m
Coordenadas
55.033, 160.725
Última erupción
950
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Composite
Roca principal
Basalt / Picro-Basalt
Resumen geológico

Komarov volcano is a complex structure along the Gamchen ridge. The summit area includes two irregular craters ~300m in diameter. Lengthy Holocene lava flows extend to the east and west. Growth began about 1,500 years ago following cessation of activity at Vysoky volcano. No reported eruptions are known, but the summit region has undergone extensive hydrothermal alteration, and fumarolic areas occur there and on the northern and southern flanks.

Resumen de Wikipedia

Resumen en inglés

Komarov is an inactive stratovolcano located in the southeastern part of the Kamchatka Peninsula, Russia. It was named after Vladimir L. Komarov.

Wikipedia · CC BY-SA · Leer artículo completo →

Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
450~500 · 1 erupciones · VEI máx. 0900~950 · 1 erupciones · VEI máx. ?450550700800900

Línea de tiempo detallada

  1. 950VEI ?Estimación geológica
    950 – En curso
  2. 450VEI 0Estimación geológica
    450 – En curso

Enlaces externos

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