Logo link to homepage

Report on Fuego (Guatemala) — 27 October-2 November 2010

Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 27 October-2 November 2010
Managing Editor: Sally Kuhn Sennert

Please cite this report as:

Global Volcanism Program, 2010. Report on Fuego (Guatemala). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 27 October-2 November 2010. Smithsonian Institution and US Geological Survey.

Volcano Profile |  Weekly Report (27 October-2 November 2010)


Fuego

Guatemala

14.473°N, 90.88°W; summit elev. 3763 m

All times are local (unless otherwise noted)


During 28-29 October, INSIVUMEH reported that explosions from Fuego produced ash plumes that rose 300-600 m above the crater. Incandescent material was ejected 75 m above the crater, and rumbling and degassing sounds were occasionally heard. Avalanches descended the W flank. On 18 October, ashfall was reported in Sangre de Cristo, 10 km WSW. Based on analyses of satellite imagery, the Washington VAAC reported that on 31 October an ash cloud was detected up to 20 km W of Fuego.

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.

Sources: Instituto Nacional de Sismologia, Vulcanologia, Meteorologia, e Hidrologia (INSIVUMEH), Washington Volcanic Ash Advisory Center (VAAC)