Kambalny
성층화산 · Russia · 2116m

- 화산 유형
- 성층화산
- 국가
- Russia
- 지역
- Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
- 해발
- 2116m
- 좌표
- 51.306, 156.875
- 마지막 분화
- 2017년
- 판구조 환경
- Subduction zone / Continental crust (> 25 km)
- 화산 지형
- Composite
- 주요 암석
- Basalt / Picro-Basalt
지질학적 요약
The southernmost major stratovolcano on the Kamchatka peninsula, Kambalny has a summit crater that is breached to the SE. Five Holocene cinder cones on the W and SE flanks have produced fresh-looking lava flows. Beginning about 6,300 radiocarbon years ago, a series of major collapses of the edifice produced at least three debris-avalanche deposits. The last major eruption took place about 600 years ago, although younger tephra layers have been found, and an eruption was reported in 1767. Active fumarolic areas are found on the flanks of the volcano, which is located south of the massive Pauzhetka volcano-tectonic depression.
Wikipedia 요약
영어 요약Kambalny is a stratovolcano located in the southern part of the Kamchatka Peninsula, Russia. It is the southernmost active volcano of Kamchatka. It has erupted mafic rocks. It has a summit crater as well as five cinder cones on its flanks which are the source of lava flows.
Wikipedia · CC BY-SA · 전체 기사 보기 →
분화 이력
상세 타임라인
- 2017년VEI 3관측 기록2017-03-24 ~ 2017-04-23Summit crater
- 1350년VEI ?지질학적 추정1350 ~ 진행 중
외부 링크
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