Report on Fuego (Guatemala) — 25 June-1 July 2003
Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 25 June-1 July 2003
Managing Editor: Gari Mayberry
Please cite this report as:
Global Volcanism Program, 2003. Report on Fuego (Guatemala). In: Mayberry, G (ed.), Weekly Volcanic Activity Report, 25 June-1 July 2003. Smithsonian Institution and US Geological Survey.
14.473°N, 90.88°W; summit elev. 3763 m
All times are local (unless otherwise noted)
Based on information from INSIVUMEH, the Washington VAAC reported that a moderate eruption began at Fuego on 29 June at 1700. Lava flows were seen, and ash fell S and SW of the volcano. As of 30 June lava flows were still visible, an ash plume was W of the summit, and seismicity was at low levels. Both days a hot spot was visible on satellite imagery, but an ash cloud could not be distinguished from abundant meteorological clouds in the area.
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.