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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: unspecified
Platanar volcano eruptions: unknown, no recent eruptions
TimeMag. / DepthDistanceLocation
Sun, 9 Dec
Sun, 9 Dec 17:48 UTCM 3.2 / 98 km13 km7 km al Norte de Tigra, San Carlos.
Tue, 27 Nov
Tue, 27 Nov 05:57 UTCM 2.7 / 5 km7 km9 km al Sur de Fortuna, San Carlos.
Fri, 23 Nov
Fri, 23 Nov 13:31 UTCM 2.8 / 8 km17 km1 km al Sur de San Isidro, V. de Coronado.
Fri, 23 Nov 08:24 UTCM 2.6 / 9 km18 km1 km al Este de Ipis, Goicoechea.
Fri, 23 Nov 04:39 UTCM 4.2 / 8 km18 km1 km al Oeste de San Isidro, V. de Coronado.
View all recent quakes

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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