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Report on Fuego (Guatemala) — 28 January-3 February 2004

Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 28 January-3 February 2004
Managing Editor: Gari Mayberry

Please cite this report as:

Global Volcanism Program, 2004. Report on Fuego (Guatemala). In: Mayberry, G (ed.), Weekly Volcanic Activity Report, 28 January-3 February 2004. Smithsonian Institution and US Geological Survey.

Volcano Profile |  Weekly Report (28 January-3 February 2004)


Fuego

Guatemala

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

All times are local (unless otherwise noted)


During 28 January to 2 February, small-to-moderate explosions occurred at Fuego. The highest rising ash plume was produced from an explosion on 29 January. The plume reached ~1.1 km above the crater and was accompanied by avalanches of volcanic material down Barranca Seca. A small amount of ash fell in Panimaché village and possibly in Santa Sofía. On 31 January two small collapses in the S edge of the central crater produced small avalanches of lava blocks.

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.

Source: Instituto Nacional de Sismologia, Vulcanologia, Meteorologia, e Hidrologia (INSIVUMEH)