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Rusia · Cono piroclástico

Cherpuk Group

Tipo
Cono piroclástico
Altitud
1868 m
Última erupción
-4550
The Yuzhny Cherpuk cinder cone (left-center horizon) and its andesitic lava flow are located 11 km SSW from Ichinsky volcano. The fresh-looking lava flow was erupted about 6,500 years ago and traveled 18 km. Severny Cherpuk (South Cherpuk) and Yuzhny Cherpuk (North Cherpuk) are two cinder cones SW of Ichinsky that comprise the largest monogenetic volcanoes of the Sredinny Range. Severny Cherpuk, 21 km SW of Ichinsky, is a double cone that was constructed along the crest of the Sredinny Range.
The Yuzhny Cherpuk cinder cone (left-center horizon) and its andesitic lava flow are located 11 km SSW from Ichinsky volcano. The fresh-looking lava flow was erupted about 6,500 years ago and traveled 18 km. Severny Cherpuk (South Cherpuk) and Yuzhny Cherpuk (North Cherpuk) are two cinder cones SW of Ichinsky that comprise the largest monogenetic volcanoes of the Sredinny Range. Severny Cherpuk, 21 km SW of Ichinsky, is a double cone that was constructed along the crest of the Sredinny Range. · Foto: Copyrighted photo by Adam Kirilenko, 2000 (Holocene Kamchatka Volcanoes, www.kamchatka.ginras.ru).
Tipo
Cono piroclástico
País
Rusia
Región
Pacífico Noroccidental / Central Kamchatka Volcanic Arc
Altitud
1868 m
Coordenadas
55.550, 157.470
Última erupción
-4550
Contexto tectónico
Zona de subducción / Corteza continental (> 25 km)
Forma volcánica
Menor
Roca principal
Andesita / Andesita basáltica
Resumen geológico

Severny Cherpuk (South Cherpuk) and Yuzhny Cherpuk (North Cherpuk) are two cinder cones SW of Ichinsky volcano that comprise the largest monogenetic volcanoes of the Sredinny Range. Severny Cherpuk, 21 km SW of Ichinsky, is a double cone that fed 1.8 km3 lava flows down both sides of the range to the NW and SE. A narrow tongue of the SE flow diverted an additional 10 km S, for a total distance of 22 km. Yuzhny Cherpuk, 11 km SSW of Ichinsky, produced a 1.7 km3 lava flow that traveled 18 km S and then SE. The flow descended to 640 m elevation and dammed tributaries of the Ketachan River, producing three lakes. The two cones are sometimes considered to be satellitic cones to Ichinsky, but Pevzner et al. (2000) noted petrological distinctions that suggest an independent origin. Unpublished radiocarbon ages revise those in Pevzner et al. (2000) and indicate that both cones were formed about 6,500 years ago.

Resumen de Wikipedia

Resumen en inglés

Cherpuk Group is a group of two cinder cones located in the central part of Kamchatka Peninsula, Russia. It is a group of a few mostly dormant cinder cones.

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Historial de erupciones

1 registradasGlosario
Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales · Usa las flechas para moverte entre barras y Enter para abrir
4550 a. C.~4550 a. C. · 1 erupciones · VEI máx. ?4550 a. C.4550 a. C.4549 a. C.4549 a. C.4549 a. C.

Línea de tiempo detallada

  1. 4550 a. C.VEI ?Estimación geológica
    4550 a. C. – fin desconocido
    North and South Cherpuk

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Enlaces externos

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