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Rusia · Maar

Kinenin

Tipo
Maar
Altitud
583 m
Última erupción
850
Kinenin maar is seen in this near-vertical aerial photo, with the lake reaching 1 km in diameter. The maar was named after the Kinenin River seen to the south, and was formed during an explosive eruption about 1,100 years ago. The NE crater wall is significantly higher and coincides with the dominant direction of the tephra dispersal.
Kinenin maar is seen in this near-vertical aerial photo, with the lake reaching 1 km in diameter. The maar was named after the Kinenin River seen to the south, and was formed during an explosive eruption about 1,100 years ago. The NE crater wall is significantly higher and coincides with the dominant direction of the tephra dispersal. · Foto: Photo from Holocene Kamchataka volcanoes (http://www.kscnet.ru/ivs/volcanoes/holocene/main/main.htm).
Tipo
Maar
País
Rusia
Región
Pacífico Noroccidental / Central Kamchatka Volcanic Arc
Altitud
583 m
Coordenadas
57.350, 160.970
Última erupción
850
Contexto tectónico
Zona de subducción / Corteza continental (> 25 km)
Forma volcánica
Menor
Roca principal
Basalto / Picrobasalto
Resumen geológico

Kinenin maar lies at the eastern foot of the Sredinny Range, about 80 km NNW of Sheveluch volcano. The 2.5-km-wide, funnel-shaped maar was formed along the Kinenin River, a tributary of the Elovka. It is partially filled by a 1-km-wide lake whose surface is at 400 m elevation. The eastern rim at about 580 m is the high point of the crater. The eruption of Kinenin took place about 1,100 years ago, making it the youngest known maar in Kamchatka. Both silicic pyroclastic flows and mafic pyroclastic ejecta were produced, which were distributed primarily to the ENE. The location is north of the active Kamchatka subduction zone.

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
850~850 · 1 erupciones · VEI máx. 4850850851851851

Línea de tiempo detallada

  1. 850 (±50 años)VEI 4Estimación geológica
    850 – fin desconocido

Volcanes cercanos

Enlaces externos

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