Hainan Dao Volcanic Field
Hainan Volcanic Field
화산대지 · China · 196m

- 화산 유형
- 화산대지
- 국가
- China
- 지역
- Eastern Asia Volcanic Regions / Southeast Asia Volcanic Province
- 해발
- 196m
- 좌표
- 19.905, 110.229
- 마지막 분화
- 1933년
- 판구조 환경
- Intraplate / Continental crust (> 25 km)
- 화산 지형
- Cluster
- 주요 암석
- Basalt / Picro-Basalt
지질학적 요약
The Hainan volcanic field consists of Quaternary lava flows that extend over about 4,100 km2 of northern Hainan Island (also known as Qiong). This field, along with the Leizhou Bandao volcanic field across the Qiongzhou strait to the north on the Leizhou (Liuchow) Peninsula, forms the larger Leiqiong volcanic field (also called the Qionglei volcano group). As many as 58 cones and craters are still evident, primarily near the city of Hainan on the north-central coast of the island. Eruptions were reported in the Lingao and Chengmai areas in the 19th and 20th centuries. Leihuling and Maanshan, two of the best preserved volcanic cones, are oriented along an E-W fracture and are part of a cluster of about 30 cones in the Shishan and Yongzing regions. The Haikou Volcanic Cluster, part of the Leiqiong World Geopark, around the town of Shishan 15 km SE of Hainan city, includes 40 volcanic features.
Wikipedia 요약
영어 요약The Hainan Volcanic Field is a 4,100 square kilometres (1,600 sq mi) volcanic field covering the northern half of Hainan, People's Republic of China. Although mostly Pleistocene-Holocene in age, minor eruptions have been recorded in the 19th and 20th centuries.
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분화 이력
상세 타임라인
- 1933년VEI ?관측 기록1933-06-26 ~ 1933-07-08Nansheling ridge
- 1883년VEI ?관측 기록1883 ~ 진행 중Lingao
외부 링크
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