Platanar
Estratovolcán · Costa Rica · 2267 m

- Tipo
- Estratovolcán
- País
- Costa Rica
- Región
- América Central y Caribe / 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
Resumen en inglésPlatanar Volcano is a dormant stratovolcano located in the Cordillera Central mountain range. It is located within Juan Castro Blanco National Park. In 1968, 2,500 hectares on Cerro Platanar were converted into a national forest.
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Historial de erupciones
Línea de tiempo detallada
No hay registros de erupciones disponibles.
Enlaces externos
⚠ Solo como referencia. No apto para respuesta ante emergencias.