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엘살바도르 · 성층화산

Cordillera de Apaneca-Lamatepec

Apaneca Range

화산 유형
성층화산
해발
2028m
마지막 분화
미확인
Cordillera de Apaneca-Lamatepec
사진: Lee Siebert, Smithsonian Institution · Public domain · Wikimedia Commons
화산 유형
성층화산
국가
엘살바도르
지역
중앙아메리카·카리브해 / Central America Volcanic Arc
해발
2028m
좌표
13.872, -89.742
마지막 분화
미확인
판구조 환경
섭입대 / 대륙 지각 (> 25 km)
화산 지형
복성화산체
주요 암석
현무암 / 피크로현무암
지질학적 요약

The Apaneca Range (also known as the Cuyanausul Range) consists of a group of basaltic-to-andesitic Pleistocene and Holocene stratovolcanoes in western El Salvador between the Santa Ana complex and the Guatemala border. The Pleistocene dacitic-rhyolitic Concepción de Ataco caldera (5 x 3.5 km) lies at the W end of the complex, along with post-caldera late-Pleistocene to Holocene andesitic-dacitic lava domes. The post-caldera cones of Cerro el Aguila (the highest peak of the complex) and Cerro los Naranjos at the E end of the chain were mapped as Holocene by Weber and Weisemann (1978). Young craters on the basaltic Cerro Laguna Verde stratovolcano may also have been active during the Holocene. Numerous fumarole fields are located on the N flank of the range, and the Ahuachapán geothermal field has been producing since 1975. Several small hydrothermal explosions have occurred in historical time, including one in October 1990 at the Agua Shuca thermal area in which 26 people were killed.

Wikipedia 요약

영어 요약

Cordillera de Apaneca is a volcanic mountain range in western El Salvador. It consists mainly of volcanoes. Ilamatepec volcano, one of the most active in the region, is a part of this range.

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