Logo link to homepage

Report on Fuego (Guatemala) — 6 January-12 January 2010

Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 6 January-12 January 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, 6 January-12 January 2010. Smithsonian Institution and US Geological Survey.

Volcano Profile |  Weekly Report (6 January-12 January 2010)


Fuego

Guatemala

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

All times are local (unless otherwise noted)


Based on analyses of satellite imagery, the Washington VAAC reported that on 6 January an ash plume from Fuego drifted 45 km SE. On 8, 11, and 12 January, INSIVUMEH reported that explosions produced ash plumes that rose to altitudes of 4-4.7 km (13,000-15,400 ft) a.s.l. Plumes drifted as far as 10 km in multiple directions, causing ashfall in some areas. Incandescent material was ejected to heights up to 75 m. Some explosions were accompanied by rumbling noises and shock waves that rattled structures up to 7 km away. Avalanches descended the flanks.

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)