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Report on Fuego (Guatemala) — 10 October-16 October 2012

Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 10 October-16 October 2012
Managing Editor: Sally Kuhn Sennert

Please cite this report as:

Global Volcanism Program, 2012. Report on Fuego (Guatemala). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 10 October-16 October 2012. Smithsonian Institution and US Geological Survey.

Volcano Profile |  Weekly Report (10 October-16 October 2012)


Fuego

Guatemala

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

All times are local (unless otherwise noted)


INSIVUMEH reported that during 10-11 October lava flows traveled 200 m down the Ceniza drainage, on Fuego's SSW flank, producing incandescent block avalanches from the flow front and steam-and-tephra plumes. On 12 October a lava flow on the S flank traveled 800 m. Explosions produced ash plumes that rose 500 m and drifted 10 km S. During 14-16 October explosions produced ash plumes that rose 400 m and drifted W and SW. A lava flow traveled 800 m down the Ceniza drainage, producing incandescent block avalanches that reached vegetated areas.

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)