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Yelovsky Volcano

Elovsky

Volcán en escudo · Russia · 1381 m

Elovsky is the highest of a cluster of small cones NE of Shishel. The Ozernovsky scoria cone (right) to the NE was the source of the massive early Holocene Ozernovsky lava flow, which traveled to the ESE down a glacial valley on the flanks of the Sredinny Range. The flow formed a lava field covering an area of 100 km2, and dammed tributary valleys, creating several lakes near the headwaters of the Levaya and Pravaya Ozernaya rivers.
Elovsky is the highest of a cluster of small cones NE of Shishel. The Ozernovsky scoria cone (right) to the NE was the source of the massive early Holocene Ozernovsky lava flow, which traveled to the ESE down a glacial valley on the flanks of the Sredinny Range. The flow formed a lava field covering an area of 100 km2, and dammed tributary valleys, creating several lakes near the headwaters of the Levaya and Pravaya Ozernaya rivers. · Foto: Copyrighted photo by Maria Pevzner, 2004 (Russian Academy of Sciences, Moscow).
Tipo
Volcán en escudo
País
Russia
Región
Northwestern Pacific Volcanic Regions / Central Kamchatka Volcanic Arc
Altitud
1381 m
Coordenadas
57.550, 160.530
Última erupción
-7550
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Shield
Roca principal
Basalt / Picro-Basalt
Resumen geológico

This cluster of overlapping small basaltic shield volcanoes is located east of the crest of the Sredinny Range, NE of Shishel and SE of Alngey volcanoes. The largest edifice is the Elovsky shield, and the smaller Ozernovsky lies immediately to the SE. The massive early Holocene Ozernovsky lava flow, located immediately NE of Elovsky, traveled to the ESE down a glacially dissected valley. The flow is post-glacial in age, but older than roughly 7,000-year-old tephra layers from Khangar volcano. The massive flow dammed tributary valleys, creating several lakes near the headwaters of the Levaya and Pravaya Ozeraya rivers and forming a lava field covering an area of 100 km2.

Resumen de Wikipedia

Resumen en inglés

Yelovsky is an extinct shield volcano in central Kamchatka. The volcano is the edifice among several overlapping small basaltic shield volcanoes. Yelovsky is located at the east of the crest of the Sredinny Range.

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Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
7550 BCE~7550 BCE · 1 erupciones · VEI máx. 47550 BCE7550 BCE7549 BCE7549 BCE7549 BCE

Línea de tiempo detallada

  1. 7550 a. C. (±500 años)VEI 4Estimación geológica
    BCE 7550 – En curso
    NE side (Ozernovsky lava flow)

Enlaces externos

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