칠레 · 성층화산
Palomo
- 화산 유형
- 성층화산
- 해발
- 4860m
- 마지막 분화
- 미확인
- 화산 유형
- 성층화산
- 국가
- 칠레
- 지역
- 남아메리카 / Southern Andean Volcanic Arc
- 해발
- 4860m
- 좌표
- -34.608, -70.295
- 마지막 분화
- 미확인
- 판구조 환경
- 섭입대 / 대륙 지각 (> 25 km)
- 화산 지형
- 복성화산체
- 주요 암석
- 안산암 / 현무암질 안산암
지질학적 요약
Palomo is a small stratovolcano that is somewhat dissected by glaciers. A NE-flank cone, Andres, is postglacial in age and has produced andesitic lava flows. The volcano lies W of the massive Caldera del Atuel and was constructed within double calderas 3 and 5 km in diameter. The largely ice-covered volcano has erupted basaltic andesite to dacitic lava flows; the double crater indicates migration of activity to the NE. The youthful morphology suggests a very recent, perhaps pre-Hispanic, age.
Wikipedia 요약
영어 요약Palomo is a 4,860 metres (15,940 ft) high Chilean stratovolcano located in the commune of Machali, Cachapoal province, Libertador General Bernardo O'Higgins Region, west of Caldera del Atuel. Together with Tinguiririca it is one of two volcanoes in the region with evidence of Holocene volcanism. The volcano is remote and knowledge on its geology and potential volcanic hazards is limited.
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