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Mascota Volcanic Field

Campo volcánico · Mexico · 2525 m

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. · Foto: Photo by Paul Wallace, 1987 (University of California Berkeley). · Wikimedia Commons
Tipo
Campo volcánico
País
Mexico
Región
Middle America-Caribbean Volcanic Regions / Trans-Mexican Volcanic Arc
Altitud
2525 m
Coordenadas
20.567, -104.817
Última erupción
Desconocido
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Cluster
Roca principal
Andesite / Basaltic Andesite
Resumen geológico

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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Enlaces externos

⚠ Solo como referencia. No apto para respuesta ante emergencias.