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Report on Santa Maria (Guatemala) — 20 January-26 January 2021

Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 20 January-26 January 2021
Managing Editor: Sally Kuhn Sennert

Please cite this report as:

Global Volcanism Program, 2021. Report on Santa Maria (Guatemala). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 20 January-26 January 2021. Smithsonian Institution and US Geological Survey.

Volcano Profile |  Weekly Report (20 January-26 January 2021)


Santa Maria

Guatemala

14.757°N, 91.552°W; summit elev. 3745 m

All times are local (unless otherwise noted)


INSIVUMEH reported that during 19-25 January explosions at Santa María's Santiaguito lava-dome complex generated ash plumes that rose 600-900 m above the complex. The extrusion of blocky lava at Caliente dome generated block-and-ash flows that mainly descended the W and SW flanks, often reaching the base of the complex. Ash plumes drifted W and SW during 20-21 January, causing ashfall in Loma Linda (6 km WSW) and San Marcos Palajunoj (8 km SW). On 22 January collapses of material to the E and SE generated pyroclastic flows.

Geologic Background. Symmetrical, forest-covered Santa María volcano is part of a chain of large stratovolcanoes that rise above the Pacific coastal plain of Guatemala. The sharp-topped, conical profile is cut on the SW flank by a 1.5-km-wide crater. The oval-shaped crater extends from just below the summit to the lower flank, and was formed during a catastrophic eruption in 1902. The renowned Plinian eruption of 1902 that devastated much of SW Guatemala followed a long repose period after construction of the large basaltic-andesite stratovolcano. The massive dacitic Santiaguito lava-dome complex has been growing at the base of the 1902 crater since 1922. Compound dome growth at Santiaguito has occurred episodically from four vents, with activity progressing W towards the most recent, Caliente. Dome growth has been accompanied by almost continuous minor explosions, with periodic lava extrusion, larger explosions, pyroclastic flows, and lahars.

Source: Instituto Nacional de Sismologia, Vulcanologia, Meteorologia, e Hidrologia (INSIVUMEH)