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Sedankinsky

Sedanka Lava Field

화산대지 · Russia · 1399m

Several scoria cones on the Sedanka Lava Field are shown in this September 2019 Planet Labs satellite image monthly mosaic (N is at the top; this image is approximately 13 km across). The Gorny Institute volcanic complex is to the upper right and the Sredny scoria cone of Tuzovsky is to the upper left, and between them are scoria cones of Sedanka. The field has more than 100 cones across an area of around 10 km.
Several scoria cones on the Sedanka Lava Field are shown in this September 2019 Planet Labs satellite image monthly mosaic (N is at the top; this image is approximately 13 km across). The Gorny Institute volcanic complex is to the upper right and the Sredny scoria cone of Tuzovsky is to the upper left, and between them are scoria cones of Sedanka. The field has more than 100 cones across an area of around 10 km. · 사진: Satellite image courtesy of Planet Labs Inc., 2019 (https://www.planet.com/).
화산 유형
화산대지
국가
Russia
지역
Northwestern Pacific Volcanic Regions / Central Kamchatka Volcanic Arc
해발
1399m
좌표
57.317, 160.067
마지막 분화
-7050년
판구조 환경
Subduction zone / Continental crust (> 25 km)
화산 지형
Cluster
주요 암석
Basalt / Picro-Basalt
지질학적 요약

The Sedanka lava field (Sedanka Dol) is located immediately west of the Sredinny Range axis and is formed by dominantly mafic lavas from small strato- and shield-like volcanoes, along with more than 100 cinder and lava cones of the late Pleistocene-Holocene age. For this compilation the volcanic field area is considered to be up to 10 km wide and stretching about 25 km from south of Gorny Institute volcano towards the NNW between Tuzovsky volcano to the SW and Titila to the NE. Other workers (eg. Nekrylov et al., 2015) define the field to include the eight large edifices from Terpuk on the SW to Shishel on the NE.

분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
7050 BCE~7050 BCE · 1건 · 최고 VEI ?7050 BCE7050 BCE7049 BCE7049 BCE7049 BCE

상세 타임라인

  1. 기원전 7050년 (±1000년)VEI ?지질학적 추정
    BCE 7050 ~ 진행 중

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