Report on Fuego (Guatemala) — 3 January-9 January 2018
Smithsonian / US Geological Survey Weekly Volcanic Activity Report,
3 January-9 January 2018
Managing Editor: Sally Kuhn Sennert
Please cite this report as:
Global Volcanism Program, 2018. Report on Fuego (Guatemala). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 3 January-9 January 2018. 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 during 4-9 January explosions at Fuego generated ash plumes that rose as high as 1.1 km above the crater and drifted mainly 10-15 km S, SW, and W, with an occasional plume moving E or NE. Some of the explosions generated shock waves. Incandescent material was ejected 100-300 m above the crater rim, causing avalanches of material that traveled within the crater and sometimes down the Ceniza (SSW), Taniluyá (SW), and Seca (W), and Las Lajas (SE) drainages. Minor ashfall was noted in local areas including Panimaché I (8 km SW), Santa Sofía (12 km SW), Morelia (9 km SW), El Porvenir, La Rochela, and Ceylon.
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)