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Mascota Volcanic Field

화산대지 · Mexico · 2525m

Volcán Tecomate (left of center) and flat-topped Volcán Molcajete (to the right), seen here from the NW, are two of the scoria cones and domes of the Mascota Volcanic Field. These are part of a group cinder cones and lava flows located within the Talpa and Mascota grabens near the town of Mascota, east of Puerto Vallarta.
Volcán Tecomate (left of center) and flat-topped Volcán Molcajete (to the right), seen here from the NW, are two of the scoria cones and domes of the Mascota Volcanic Field. These are part of a group cinder cones and lava flows located within the Talpa and Mascota grabens near the town of Mascota, east of Puerto Vallarta. · 사진: Photo by Paul Wallace, 1987 (University of California Berkeley). · Wikimedia Commons
화산 유형
화산대지
국가
Mexico
지역
Middle America-Caribbean Volcanic Regions / Trans-Mexican Volcanic Arc
해발
2525m
좌표
20.567, -104.817
마지막 분화
미확인
판구조 환경
Subduction zone / Continental crust (> 25 km)
화산 지형
Cluster
주요 암석
Andesite / Basaltic Andesite
지질학적 요약

A group of calc-alkaline andesitic and lamprophyre cinder cones and lava domes, along with associated lava flows, is located near the town of Mascota about 50 km E of Puerto Vallarta. Mascota is the youngest of a group of potassic volcanic fields in extensional grabens of the Jalisco block south of the Río Ameca. Most volcanism here is confined to two NNW-SSE-trending grabens cutting Cretaceous ash-flow tuffs. The youngest eruption was a basaltic andesite lava flow at Volcán Malpaís, north of Mascota; the lack of soil development and sparse vegetation suggest that it may be only a few thousand years old (Carmichael et al., 1996). The field is noted for its unusual diversity of volcanic rocks, and contains Earth's youngest known minettes (lamprophyres).

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