Volcán Tajumulco

Tajumulco is composed of andesitic-dacitic lavas on the top of a large escarpment of uncertain origin. It has two summits, one of which has a crater wide. A lava flow from the north-western summit descends into a steep valley on the same side of the volcano. The volcano's eruptive history is unclear and the date of its last eruption unknown. Reports from the 18th and early 19th century claim to record eruptions but these are considered unlikely. ==See also==