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Yelovsky Volcano

Elovsky

Tipe
Gunung api perisai
Ketinggian
1381 m
Letusan terakhir
-7550
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).
Tipe
Gunung api perisai
Negara
Rusia
Wilayah
Pasifik Barat Laut / Central Kamchatka Volcanic Arc
Ketinggian
1381 m
Koordinat
57.550, 160.530
Letusan terakhir
-7550
Kondisi tektonik
Zona subduksi / Kerak benua (> 25 km)
Bentuk lahan
Perisai
Batuan utama
Basal / Pikrobasal
Ringkasan geologi

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.

Ringkasan Wikipedia

Ringkasan Inggris

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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7550 SM~7550 SM · 1 letusan · VEI maks. 47550 SM7550 SM7549 SM7549 SM7549 SM

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  1. 7550 SM (±500 tahun)VEI 4Perkiraan geologi
    7550 SM – akhir tidak diketahui
    NE side (Ozernovsky lava flow)

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