본문으로 건너뛰기

아과스 칠리케스산

Chiliques

성층화산 · Chile · 5778m

Snow-capped Volcán Chiliques is a conical stratovolcano located NNE of Laguna Miscanti (foreground).  The 5778-m-high summit of the volcano contains a 500-m-wide crater.  Several youthful lava flows, some of which are considered to be of Holocene age descend its flanks.  Chiliques had previously been considered to be dormant; however, in 2002 a NASA nighttime thermal infrared satellite image showed low-level hot spots in the summit crater and upper flanks.
Snow-capped Volcán Chiliques is a conical stratovolcano located NNE of Laguna Miscanti (foreground). The 5778-m-high summit of the volcano contains a 500-m-wide crater. Several youthful lava flows, some of which are considered to be of Holocene age descend its flanks. Chiliques had previously been considered to be dormant; however, in 2002 a NASA nighttime thermal infrared satellite image showed low-level hot spots in the summit crater and upper flanks. · 사진: Photo by Carlos Felipe Ramírez (courtesy of Oscar González-Ferrán, University of Chile). · Wikimedia Commons
화산 유형
성층화산
국가
Chile
지역
South America Volcanic Regions / Central Andean Volcanic Arc
해발
5778m
좌표
-23.580, -67.700
마지막 분화
미확인
판구조 환경
Subduction zone / Continental crust (> 25 km)
화산 지형
Composite
주요 암석
Andesite / Basaltic Andesite
지질학적 요약

Volcán Chiliques is a structurally simple stratovolcano located immediately south of Laguna Lejía. The summit contains a 500-m-wide crater. Several youthful lava flows, some of which are considered to be of possible Holocene age (de Silva, 2007 pers. comm.), descend its flanks. The largest of these extends 5 km NW. Older lava flows reach up to 10 km from the summit on the N flank. This volcano had previously been considered to be dormant; however, in 2002 a NASA nighttime thermal infrared satellite image from the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) showed low-level hot spots in the summit crater and upper flanks.

Wikipedia 요약

아과스 칠리케스 산(Aguas Chiliques)은 칠레의 안토파가스타에 놓여있는 안산암질 성층 화산이다. 이 화산은 라스카르 화산과 함께 이웃해 있으며, 화산활동은 많이 없지만 활동을 재개할 가능성이 보인다. 라스카르 화산과 붙어 있고 아래에는 염호가 있다. 분화구는 작고, 오랫동안 분화한 기록이 없지만 곧 분화를 다시 할 수 가 있다.

Wikipedia · CC BY-SA · 전체 기사 보기

분화 이력

상세 타임라인

분화 기록이 없습니다.

외부 링크

⚠ 참고용 정보입니다. 재난 대응에 사용하지 마세요.