
OTHER NAMES USED
ALTITUDE
TYPE OF EDIFICECerro Quemado is an exogenous lava dome consisting of an overlapping sequence of viscous dacite block lava flows. La Pedrera, a pumicious rhyodacite lava flow just north of Cerro Quemado, is probably only slightly older than Cerro Quemado. Cerro Quemado is located on the west rim of an apparent ring crater marked by other domes, called Volcán Almolonga by Johns (1975). Cerro Quemado is surrounded by other volcanoes, included Santo Tomas, Santa María and Santiaguito, Siete Orejas, and Chicabal. The Quezaltenango Valley north of Cerro Quemado is possibly a large caldera (Duffield et al., 1991).

LOCATION/GEOLOGICAL SETTING
HOW TO GET THERE
TOPOGRAPHIC MAPS/AIR PHOTOS
PETROLOGY
ERUPTION HISTORY/AGE OF THE VOLCANISM
DOMES AND FLOWS OF CERRO QUEMADO
MASSIVE COLLAPSE OF CERRO QUEMADO 1200 YEARS AGO
VOLCANIC ASH IN ANCIENT MAYA CERAMICS
BIBLIOGRAPHY