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Platanar

Estratovolcán · Costa Rica · 2267 m

The Platanar volcanic complex on the horizon is the NW-most volcano in the Cordillera Central of Costa Rica. The complex consists of Platanar and Porvenir, which formed within the Chocosuela caldera. This view is from the east with the Hule maar, located about 11 km north of the Poás summit, in the foreground.
The Platanar volcanic complex on the horizon is the NW-most volcano in the Cordillera Central of Costa Rica. The complex consists of Platanar and Porvenir, which formed within the Chocosuela caldera. This view is from the east with the Hule maar, located about 11 km north of the Poás summit, in the foreground. · Foto: Photo by Mike Carr, 1983 (Rutgers University). · Wikimedia Commons
Tipo
Estratovolcán
País
Costa Rica
Región
Middle America-Caribbean Volcanic Regions / Central America Volcanic Arc
Altitud
2267 m
Coordenadas
10.300, -84.366
Última erupción
Desconocido
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Composite
Roca principal
Andesite / Basaltic Andesite
Resumen geológico

The Platanar volcanic center is the NW-most volcano in the Cordillera Central of Costa Rica. The massive complex covers about 900 km2 and is dominated by two largely Pleistocene stratovolcanoes, Platanar and Porvenir. These volcanoes were constructed within the Pleistocene Chocosuela caldera, which may have formed during a major slope failure. The Cerro Platanar volcano (known locally as Volcán Congo) on the N side of the complex has prehistorical lava flows on its W flanks and is the youngest volcanic center. The highest peak is Porvenir, whose summit crater lies 3 km S of Platanar. A thin layer of phreatic ash suggested that an eruption from Platanar occurred within the past few thousand years (Stine and Banks, 1991). The Aguas Zarcas group of nine basaltic cinder cones, located on the N flank of the Platanar-Porvenir complex to as low as 160 m altitude is, in part, Holocene in age.

Resumen de Wikipedia

El volcán Platanar, también conocido como "cerro Congo", es un estratovolcán inactivo, localizado a 8 km al sudeste de Ciudad Quesada, San Carlos, Costa Rica, en la Cordillera Volcánica Central. Este volcán se encuentra protegido dentro del Parque Nacional Juan Castro Blanco.

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