PANAMA VOLCANIC HISTORY

 There are three volcanoes located in Panama; Baru with its last eruption in 1550, El Valle being Holocene, & La Yeguada in 1620. "Central Panama, considered here as the area close to the Panama Canal between El Valle volcano and Cerro Azul mountains , is characterised by a unique geomorphology and geology in the Panama Isthmus. This area consists of lowlands punctuated by small (generally <300 m high) topographic features of unclear tectonic and/or volcanic origins . It corresponds to a major topographic discontinuity between higher volcanic cordilleras that form the most prominent topography in the east and west. Lineament analysis, geophysical constraints, palaeomagnetic data, and field observations show that the unique topography of Central Panama is at least in part controlled by a complex fault network associated with crustal-scale dismemberment of transisthmian volcanic cordilleras since the Late Eocene. However, it remains poorly constrained whether topographic highs in Central Panama represent erosional remnants of ancient volcanic landforms that could have obstructed/closed an interoceanic strait in this area" (nature.com) 










https://en.wikipedia.org/wiki/List_of_volcanoes_in_Panama 

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