Kunlun Volcanic Group
Ashikule Volcanic Field
화산대지 · China · 5090m

- 화산 유형
- 화산대지
- 국가
- China
- 지역
- Eastern Asia Volcanic Regions / Northern Tibetan Plateau Volcanic Province
- 해발
- 5090m
- 좌표
- 35.742, 81.646
- 마지막 분화
- 1951년
- 판구조 환경
- Intraplate / Continental crust (> 25 km)
- 화산 지형
- Cluster
- 주요 암석
- Trachyte / Trachydacite
지질학적 요약
The Ashikule Volcanic Field contains 10 Pliocene to Holocene pyroclastic cones at the western end of the Kunlun Mountains. Several young trachyandesitic cones lie in the area around Ashi (Aqqikkol) and Wuluke (Ulugkol) lakes. China's most recent eruption was observed by a road-building crew on 27 May 1951, at the Ashishan (also known as Ka-er-daxi or Vulkan) cone. The eruption began with a loud detonation and ejected large blocks, emitting "smoke" for a number of days. An unconfirmed eruption was reported in the 19th century.
Wikipedia 요약
영어 요약Kunlun Volcanic Group, also known as Ashiköli Volcanic Field, is a volcanic field in northwestern Tibet. Eight other volcanic fields are also in the area. The field is within a basin that also contains three lakes.
Wikipedia · CC BY-SA · 전체 기사 보기 →
분화 이력
상세 타임라인
- 1951년VEI 2관측 기록1951-05-27 ~ 진행 중Ashi Shan
- 1850년 (±50년)VEI ?지질학적 추정1850 ~ 진행 중
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