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Miravalles volcano

Stratovolcano 2028 m / 6,653 ft
Costa Rica, 10.75°N / -85.15°W
Current status: dormant (1 out of 5) | Reports
Miravalles volcano books
Typical eruption style: unspecified
Miravalles volcano eruptions: 1946 
TimeMag. / DepthDistanceLocation
Mon, 16 Apr
Mon, 16 Apr 19:13 UTCM 2.8 / 5 km8 km2 km al Este de Bijagua, Upala.
Mon, 16 Apr 19:05 UTCM 2.9 / 5 km8 km0 km al Noreste de Bijagua, Upala.
Fri, 13 Apr
Fri, 13 Apr 09:55 UTCM 2.8 / 3 km3 km6 km al Sureste de Bijagua, Upala.
Fri, 13 Apr 09:04 UTCM 2.8 / 9 km4 km4 km al Sureste de Bijagua, Upala.
Thu, 12 Apr
Thu, 12 Apr 18:37 UTCM 3.6 / 5 km5 km3 km al Sur de Bijagua, Upala.
View all recent quakes

Background:

Miravalles is a 2028-m-high andesitic stratovolcano that is one of five post-caldera cones along a NE-trending line within the broad 15 x 20 km Guayabo (Miravalles) caldera. The caldera was formed during several major explosive eruptions that produced voluminous dacitic-rhyolitic pyroclastic flows between about 1.5 and 0.6 million years ago. Growth of post-caldera volcanoes in the eastern part of the caldera that overtopped much of the eastern and southern caldera rims was interrupted by edifice collapse that produced a major debris avalanche to the SW. Morphologically youthful lava flows cover the western and SW flanks of the post-caldera Miravalles complex, which rises above the town of Guayabo on the flat western caldera floor. The only reported historical eruptive activity was a small steam explosion on the SW flank in 1946. High heat flow remains, and Miravalles is the site of the largest developed geothermal field in Costa Rica.
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Smithsonian / GVP volcano information


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