Platanar
Stratovulcano · Costa Rica · 2267 m

- Tipo
- Stratovulcano
- Paese
- Costa Rica
- Regione
- Middle America-Caribbean Volcanic Regions / Central America Volcanic Arc
- Altitudine
- 2267 m
- Coordinate
- 10.300, -84.366
- Ultima eruzione
- Sconosciuto
- Contesto tettonico
- Subduction zone / Continental crust (> 25 km)
- Forma vulcanica
- Composite
- Roccia principale
- Andesite / Basaltic Andesite
Sintesi geologica
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.
Sintesi da Wikipedia
Riassunto in inglesePlatanar 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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Storia delle eruzioni
Cronologia dettagliata
Nessuna registrazione di eruzioni disponibile.
Link esterni
⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.