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Ushkovsky

Volcán compuesto · Russia · 3943 m

Ushkovsky is a large compound volcanic massif located at the NW end of the Klyuchevskaya volcano group. Seen here from the NW, it consists of the flat-topped Ushkovsky (far right), which is capped by an ice-filled 4.5 x 5.5 km caldera, and the adjacent higher Krestovsky peak (center). Numerous scoria cones have formed on its flanks.
Ushkovsky is a large compound volcanic massif located at the NW end of the Klyuchevskaya volcano group. Seen here from the NW, it consists of the flat-topped Ushkovsky (far right), which is capped by an ice-filled 4.5 x 5.5 km caldera, and the adjacent higher Krestovsky peak (center). Numerous scoria cones have formed on its flanks. · Foto: Photo by E.Y. Zhdanova (courtesy of Oleg Volynets, Institute of Volcanology, Petropavlovsk). · Wikimedia Commons
Tipo
Volcán compuesto
País
Russia
Región
Northwestern Pacific Volcanic Regions / Eastern Kamchatka Volcanic Arc
Altitud
3943 m
Coordenadas
56.113, 160.509
Última erupción
1890
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Composite
Roca principal
Basalt / Picro-Basalt
Resumen geológico

The Ushkovsky (formerly known as Plosky) complex is a large compound volcanic massif located at the NW end of the Kliuchevskaya volcano group. The summit of Krestovsky (Blizhny Plosky) volcano, about 10 km NW of Kliuchevskoy, is the high point of the complex. Linear zones of cinder cones are found on the SW and NE flanks and on lowlands to the west. The Ushkovsky (Daljny Plosky) edifice SE of Krestkovsky is capped by an ice-filled 4.5 x 5.5 km caldera containing two glacier-clad cinder cones with large summit craters. A younger caldera at the summit of Daljny was formed in association with the eruption of large lava flows and pyroclastic material from the Lavovy Shish cinder cones at the foot of the volcano about 8,600 years ago. An explosive eruption took place from the summit cone in 1890.

Resumen de Wikipedia

Resumen en inglés

Ushkovsky is a large volcanic massif located in the central part of the Kamchatka Peninsula, Russia. It is located at the northwestern end of the Klyuchevskaya Sopka volcano group. These volcanoes are also set in a chain linked formation. The highest peak of this massif is Krestovsky. Krestovsky is a stratovolcano, Ushkovsky is a shield volcano.

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Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
7550 BCE~7235 BCE · 1 erupciones · VEI máx. ?6921 BCE~6606 BCE · 1 erupciones · VEI máx. ?1575~1890 · 1 erupciones · VEI máx. 27550 BCE5347 BCE2830 BCE627 BCE1575

Línea de tiempo detallada

  1. 1890VEI 2Observado
    1890-04 – En curso
  2. 6670 a. C. (±150 años)VEI ?Estimación geológica
    BCE 6670 – En curso
    Lavovy Shish cone group & summit caldera
  3. 7550 a. C.VEI ?Estimación geológica
    BCE 7550 – En curso

Enlaces externos

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