Report on Santa Maria (Guatemala) — 20 February-26 February 2013
Smithsonian / US Geological Survey Weekly Volcanic Activity Report,
20 February-26 February 2013
Managing Editor: Sally Kuhn Sennert
Please cite this report as:
Global Volcanism Program, 2013. Report on Santa Maria (Guatemala). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 20 February-26 February 2013. Smithsonian Institution and US Geological Survey.
14.757°N, 91.552°W; summit elev. 3745 m
All times are local (unless otherwise noted)
INSIVUMEH reported that during 20-21 February an explosion from Santa María's Santiaguito lava-dome complex produced an ash plume that rose 600 m and caused ashfall in the region of Palajunoj, on the SW flank, and in La Florida (5 km S). Steam plumes rose 200 m and drifted SW, and avalanches from lava-flow fronts traveled NE. On 22 February an explosion produced an ash plume that rose 800 m and drifted SW, causing ashfall in Monte Claro (S). Avalanches from lava-flow fronts traveled SE. A change in the wind direction on 23 February blew ash plumes N, generated ashfall in Quetzaltenango (18 km WNW). Explosions during 24-25 February generated ash plumes that rose 500 m and drifted E. Avalanches descended the S and SE flanks.
Geological Summary. 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.