본문으로 건너뛰기

Atlasov

Nylgimelkin

순상화산 · Russia · 1764m

This cone formed at the top of Nylgimelkin, with the larger Pleistocene Khuvkhoitun volcano visible in the background. Lava flows from Nylgimelkin were erupted along a fissure about 5,500 years ago.
This cone formed at the top of Nylgimelkin, with the larger Pleistocene Khuvkhoitun volcano visible in the background. Lava flows from Nylgimelkin were erupted along a fissure about 5,500 years ago. · 사진: Copyrighted photo by Maria Pevzner, 2005 (Russian Academy of Sciences, Moscow).
화산 유형
순상화산
국가
Russia
지역
Northwestern Pacific Volcanic Regions / Central Kamchatka Volcanic Arc
해발
1764m
좌표
57.970, 160.650
마지막 분화
-3550년
판구조 환경
Subduction zone / Continental crust (> 25 km)
화산 지형
Shield
주요 암석
Basalt / Picro-Basalt
지질학적 요약

The basaltic Nylgimelkin (also known as Atlasov) shield volcano and the topographically higher but smaller shield of Novagrablenova are dwarfed by their neighbor, the glacier-clad Pleistocene Khuvkhoitun, the highest Quaternary volcano of the northern Sredinny Range. The two youthful shields were constructed on the W and NW flanks of Khuvkhoitun. Lava flows from them extend primarily to the west. Cinder cones and a lava flow were erupted along a fissure at Nylgimelkin about 5,500 years ago.

Wikipedia 요약

영어 요약

Atlasova is a basaltic shield volcano situated in Kamchatka. It is named after Russian explorer Vladimir Atlasov.

Wikipedia · CC BY-SA · 전체 기사 보기

분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
3550 BCE~3550 BCE · 1건 · 최고 VEI ?3550 BCE3550 BCE3549 BCE3549 BCE3549 BCE

상세 타임라인

  1. 기원전 3550년VEI ?지질학적 추정
    BCE 3550 ~ 진행 중

외부 링크

⚠ 참고용 정보입니다. 재난 대응에 사용하지 마세요.