Report on Tacana (Mexico-Guatemala) — January 1987
Scientific Event Alert Network Bulletin, vol. 12, no. 1 (January 1987)
Managing Editor: Lindsay McClelland..
Tacana (Mexico-Guatemala) Seismic swarms
Please cite this report as:
Global Volcanism Program, 1987. Report on Tacana (Mexico-Guatemala). In: McClelland, L. (ed.), Scientific Event Alert Network Bulletin, 12:1. Smithsonian Institution. https://doi.org/10.5479/si.GVP.SEAN198701-341130.
15.132°N, 92.109°W; summit elev. 4064 m
All times are local (unless otherwise noted)
Three seismic swarms in the vicinity of Tacaná were recorded 20-28 January [see also 12:3]. Two began with magnitude 3 events. During a swarm that began 25 January, about 35 microearthquakes occurred/hour, with 750 events (M <1) recorded 25-26 January. The velocity model for the area remains uncertain, precluding precise hypocenter determinations, but events from the 25-26 January swarm appeared to be at 5-10 km depth. Geologists suspected that the seismicity may have been tectonic. No change in activity at the volcano has been reported.
Geologic Background. Tacaná is a 4064-m-high composite stratovolcano that straddles the México/Guatemala border at the NW end of the Central American volcanic belt. The volcano rises 1800 m above deeply dissected plutonic and metamorphic terrain. Three large calderas breached to the south, and the elongated summit region is dominated by a series of lava domes intruded along a NE-SW trend. Volcanism has migrated to the SW, and a small adventive lava dome is located in the crater of the youngest volcano, San Antonio, on the upper SW flank. Viscous lava flow complexes are found on the north and south flanks, and lobate lahar deposits fill many valleys. Radial drainages on the Guatemalan side are deflected by surrounding mountains into the Pacific coastal plain on the SW side of the volcano. Historical activity has been restricted to mild phreatic eruptions, but more powerful explosive activity, including the production of pyroclastic flows, has occurred as recently as about 1950 years ago.
Information Contacts: E. Sánchez, INSIVUMEH; Norman Banks and Michael Doukas, USGS CVO.