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Yelovsky Volcano

Elovsky

순상화산 · Russia · 1381m

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. · 사진: Copyrighted photo by Maria Pevzner, 2004 (Russian Academy of Sciences, Moscow).
화산 유형
순상화산
국가
Russia
지역
Northwestern Pacific Volcanic Regions / Central Kamchatka Volcanic Arc
해발
1381m
좌표
57.550, 160.530
마지막 분화
-7550년
판구조 환경
Subduction zone / Continental crust (> 25 km)
화산 지형
Shield
주요 암석
Basalt / Picro-Basalt
지질학적 요약

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.

Wikipedia 요약

영어 요약

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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분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
7550 BCE~7550 BCE · 1건 · 최고 VEI 47550 BCE7550 BCE7549 BCE7549 BCE7549 BCE

상세 타임라인

  1. 기원전 7550년 (±500년)VEI 4지질학적 추정
    BCE 7550 ~ 진행 중
    NE side (Ozernovsky lava flow)

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