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Platanar volcano

Stratovolcanoes 2267 m / 7,438 ft
Costa Rica, 10.3°N / -84.37°W
Current status: normal or dormant (1 out of 5) | Reports
Platanar volcano books
Typical eruption style: sin especificar
Erupciones del volcán Platanar: unknown, no recent eruptions
Fecha / HoraRevista / ProfundidadDistanciaUbicación
Mon, 14 Jan
Mon, 14 Jan 05:56 UTCM 3.2 / 79 km15 km2 km al Sureste de San Isidro, Heredia.
Fri, 4 Jan
Fri, 4 Jan 10:36 UTCM 3.5 / 89 km11 km4 km al Sur de Rio Cuarto, Alajuela.
Tue, 1 Jan
Tue, 1 Jan 12:39 UTCM 3.3 / 77 km1 km8 km al Sureste de Varablanca, Heredia.
Fri, 28 Dec
Fri, 28 Dec 19:28 UTCM 2.9 / 89 km14 km14 km al Noreste de Varablanca, Heredia.
Wed, 26 Dec
Wed, 26 Dec 21:05 UTCM 3.5 / 84 km11 km6 km al Suroeste de Ciudad Quesada.
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Background:

The Platanar volcanic center is the NW-most volcano in the Cordillera Central of Costa Rica. The massive complex covers about 900 sq km 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 2183-m-high Cerro Platanar volcano (known locally as Volcán Congo) on the north side of the complex has prehistorical lava flows on its western flanks and is the youngest volcanic center. The highest peak of the complex is 2267-m-high Porvenir volcano, whose summit crater lies 3 km south 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 north flank of the Platanar-Porvenir complex to as low as 160 m altitude, is in part Holocene in age.
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Smithsonian / GVP volcano information


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