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Elovskij

Elovsky

Vulcano a scudo · 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
Vulcano a scudo
Paese
Russia
Regione
Northwestern Pacific Volcanic Regions / Central Kamchatka Volcanic Arc
Altitudine
1381 m
Coordinate
57.550, 160.530
Ultima eruzione
-7550
Contesto tettonico
Subduction zone / Continental crust (> 25 km)
Forma vulcanica
Shield
Roccia principale
Basalt / Picro-Basalt
Sintesi geologica

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.

Sintesi da Wikipedia

Riassunto breve — apri l'articolo completo per maggiori dettagli.

L'Elovskij è un vulcano a scudo situato nella Kamčatka centrale.

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Storia delle eruzioni

Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni
7550 BCE~7550 BCE · 1 eruzioni · VEI max. 47550 BCE7550 BCE7549 BCE7549 BCE7549 BCE

Cronologia dettagliata

  1. 7550 a.C. (±500 anni)VEI 4Stima geologica
    BCE 7550 – In corso
    NE side (Ozernovsky lava flow)

Link esterni

⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.