그라시오자섬
Graciosa
성층화산 · Portugal · 402m

- 화산 유형
- 성층화산
- 국가
- Portugal
- 지역
- 대서양 / Azores-Terceira Rift Volcanic Province
- 해발
- 402m
- 좌표
- 39.020, -27.970
- 마지막 분화
- -1950년
- 판구조 환경
- Rift zone / Oceanic crust (< 15 km)
- 화산 지형
- Composite
- 주요 암석
- Basalt / Picro-Basalt
지질학적 요약
The SE end of Graciosa, the northernmost of the central Azorean islands, contains a 0.9 x 1.6 km caldera with active fumaroles. The SE caldera rim is the high point of the 7 x 12 km island. The caldera has been the source of eruptions producing significant tephra falls, pyroclastic flows, lahars, and lava flows. Fumaroles are present in a volcanic cave inside the caldera, and a submarine fumarole occurs off the NW coast. Scoria cones erupted along several widely spaced NE-SW-trending fissures fed a youthful lava field that forms the NW end of the island. The most recent eruption from Pico Tomao, NW of the caldera, produced a lava flow during the mid-to-late Holocene that reached the eastern coast NW of the village of Praia.
Wikipedia 요약
영어 요약Graciosa Island, also referred to as the White Island, is a volcanic island in the Atlantic Ocean. It is the northernmost of the Central Group of islands in the Azores archipelago. The ovular Portuguese island has an area of 60.65 square kilometres, a length of 10 kilometres and a width of 7 kilometres. Its landscape is dominated by a 1.6-kilometre-wide (1.0-mile) central caldera located in the southeast.
Wikipedia · CC BY-SA · 전체 기사 보기 →
분화 이력
상세 타임라인
- 기원전 1950년 (±1400년)VEI ?지질학적 추정BCE 1950 ~ 진행 중San Tamao
외부 링크
⚠ 참고용 정보입니다. 재난 대응에 사용하지 마세요.