frequently visible from
Guatemala City, the nation's
capital. Pacaya is a complex
basaltic volcano constructed
just outside the southern
topographic rim of the 14 x
16 km Pleistocene Amatitlán
caldera. A cluster of dacitic
lava domes occupies the
southern caldera floor. The
post-caldera Pacaya massif
includes the Cerro Grande
lava dome and a younger
volcano to the SW. Collapse of Pacaya volcano about 1100 years ago
produced a debris-avalanche deposit that extends 25 km onto the Pacific
coastal plain and left an arcuate somma rim inside which the modern Pacaya
volcano (MacKenney cone) grew. A subsidiary crater, Cerro Chino, was
constructed on the NW somma rim and was last active in the 19th century.
During the past several decades, activity at Pacaya has consisted of frequent
strombolian eruptions with intermittent lava flow extrusion that has partially
filled in the caldera moat and armored the flanks of MacKenney cone,
punctuated by occasional larger explosive eruptions that partially destroy the
summit of the cone. (Global Volcanism Program)
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