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San Vicente

성층화산 · El Salvador · 2149m

San Vicente is seen here from the north along the Pan-American highway. Numerous hot springs and fumaroles are found on its flanks.
San Vicente is seen here from the north along the Pan-American highway. Numerous hot springs and fumaroles are found on its flanks. · 사진: Photo by Kristal Dorion, 1994 (U.S. Geological Survey). · Wikimedia Commons
화산 유형
성층화산
국가
El Salvador
지역
중앙아메리카·카리브해 / Central America Volcanic Arc
해발
2149m
좌표
13.597, -88.838
마지막 분화
미확인
판구조 환경
Subduction zone / Continental crust (> 25 km)
화산 지형
Composite
주요 암석
Andesite / Basaltic Andesite
지질학적 요약

San Vicente stratovolcano, also known as Chichontepec, is ~20 km SE of Lake Ilopango. The andesitic edifice with two summit peaks was constructed within the Pleistocene La Carbonera caldera, whose rim is visible only on its SW side. The N and S flanks are covered by lava flows from the central vent, but lava flows on the eastern side originated from a vent on the upper flank. Volcanism has continued into the Holocene, but the latest lava flows are covered by deposits from the major Tierra Blanca eruption from Ilopango around 450 CE. Reports of eruptions in 1643 CE and 1835 CE are false (Catalog of Active Volcanoes of the World; Sapper, 1917), but numerous hot springs and fumaroles are found on the N and W flanks.

분화 이력

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