Report on Fuego (Guatemala) — February 1991
Bulletin of the Global Volcanism Network, vol. 16, no. 2 (February 1991)
Managing Editor: Lindsay McClelland.
Fuego (Guatemala) Prominent plume; moderate SO2 emission
Please cite this report as:
Global Volcanism Program, 1991. Report on Fuego (Guatemala). In: McClelland, L. (ed.), Bulletin of the Global Volcanism Network, 16:2. Smithsonian Institution. https://doi.org/10.5479/si.GVP.BGVN199102-342090.
14.473°N, 90.88°W; summit elev. 3763 m
All times are local (unless otherwise noted)
During an aerial survey on 10 February, no changes in crater morphology were evident since the previous overflight a year earlier (15:03). The plume remained prominent, and SO2 emission measured by COSPEC was 190 ± 21 t/d.
Geologic Background. Volcán Fuego, one of Central America's most active volcanoes, is one of three large stratovolcanoes overlooking Guatemala's former capital, Antigua. The scarp of an older edifice, Meseta, lies between 3763-m-high Fuego and its twin volcano to the north, Acatenango. Construction of Meseta dates back to about 230,000 years and continued until the late Pleistocene or early Holocene. Collapse of Meseta may have produced the massive Escuintla debris-avalanche deposit, which extends about 50 km onto the Pacific coastal plain. Growth of the modern Fuego volcano followed, continuing the southward migration of volcanism that began at Acatenango. In contrast to the mostly andesitic Acatenango, eruptions at Fuego have become more mafic with time, and most historical activity has produced basaltic rocks. Frequent vigorous historical eruptions have been recorded since the onset of the Spanish era in 1524, and have produced major ashfalls, along with occasional pyroclastic flows and lava flows.
Information Contacts: Rodolfo Morales and Gustavo Chigna, Sección de Vulcanología, INSIVUMEH; W.I. Rose, Robert Andres, and Kimberly Kogler, Michigan Technological Univ., USA.