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Report on Fuego (Guatemala) — 30 March-5 April 2022


Fuego

Smithsonian / US Geological Survey Weekly Volcanic Activity Report,
30 March-5 April 2022
Managing Editor: Sally Kuhn Sennert

Please cite this report as:

Global Volcanism Program, 2022. Report on Fuego (Guatemala). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 30 March-5 April 2022. Smithsonian Institution and US Geological Survey.

Weekly Report (30 March-5 April 2022)

Fuego

Guatemala

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

All times are local (unless otherwise noted)


INSIVUMEH reported that 4-8 explosions per hour were detected at Fuego during 30 March through 5 April, generating gas-and-ash emissions that rose to 4.9 km (16,000 ft) a.s.l. and drifted as far as 30 km NW, W, SW, and S. Block avalanches descended the Las Lajas (SE), Seca (W), Ceniza (SSW), Taniluyá (SW), Trinidad (S), Honda, and Santa Teresa drainages. At night, incandescence was observed up to 150 m above the crater. Fine ashfall was reported in Panimaché I and II (8 km SW), Morelia (9 km SW), Santa Sofía (12 km SW), Finca Palo Verde, Yepocapa (8 km NW), El Porvenir (8 km ENE), and Sangre de Cristo (8 km WSW). Shock waves from the explosions and rumbling sounds rattled local structures. Based on satellite and wind model data, the Washington VAAC reported that during 29 March through 4 April ash plumes from Fuego rose to 4.9 km (16,000 ft) a.s.l. and drifted SE, E, SW, S, WNW, WSW.

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.

Sources: Instituto Nacional de Sismologia, Vulcanologia, Meteorologia, e Hidrologia (INSIVUMEH), Coordinadora Nacional para la Reducción de Desastres (CONRED), Washington Volcanic Ash Advisory Center (VAAC)