Report on Fuego (Guatemala) — 2 July-8 July 2003
Smithsonian / US Geological Survey Weekly Volcanic Activity Report,
2 July-8 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, 2 July-8 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)
INSIVUMEH reported that the eruption at Fuego on 29 June during 1745-2200 consisted mainly of lava flows and avalanches of volcanic material traveling down the volcano's E flank. Incandescence was visible from the city of Antigua and the S coast. Ash fell in villages W and SE of the volcano, including San Pedro Yepocapa. Explosions and tremor were recorded by a seismic station. After the eruption, weak-to-moderate explosions at Fuego produced ash clouds to ~900 m above the volcano and seismographs mainly recorded tremor. Pyroclastic-flow material extended ~1.5 km down the volcano's W flank. Fuego was at Alert Level Yellow and pilots were advised to avoid flying near the volcano.
Geological Summary. Volcán Fuego, one of Central America's most active volcanoes, is also one of three large stratovolcanoes overlooking Guatemala's former capital, Antigua. The scarp of an older edifice, Meseta, lies between Fuego and Acatenango to the north. 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 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)