Report on Irazu (Costa Rica) — January 1991
Bulletin of the Global Volcanism Network, vol. 16, no. 1 (January 1991)
Managing Editor: Lindsay McClelland.
Irazu (Costa Rica) Nearby seismic swarm apparently tectonic; surface activity unchanged
Please cite this report as:
Global Volcanism Program, 1991. Report on Irazu (Costa Rica) (McClelland, L., ed.). Bulletin of the Global Volcanism Network, 16:1. Smithsonian Institution. https://doi.org/10.5479/si.GVP.BGVN199101-345060
9.979°N, 83.852°W; summit elev. 3432 m
All times are local (unless otherwise noted)
A seismic swarm, centered between San Juan de Chicuá and the summit (figure 1), began on 2 January and continued through the end of the month. Two peaks in swarm activity occurred, the first on 7 January when 95 events were recorded, and the second on 27 January with 103 events (figure 2); 700 were recorded during the month. Seismicity increased towards the end of January, with maximum magnitudes of 4.0 (table 2) and intensities of MM III-IV. Several of the shocks were felt by area residents.
|Figure 1. Epicenters of earthquakes recorded during the January 1991 seismic swarm at Irazú. Courtesy of Gerardo Soto.|
|07 Jan 1991||1011||2.1|
|07 Jan 1991||1013||2.1|
|07 Jan 1991||1234||2.5|
|07 Jan 1991||1352||2.7|
|08 Jan 1991||0407||3.3|
|13 Jan 1991||1017||3.5|
|16 Jan 1991||0708||3.8|
|16 Jan 1991||0748||2.0|
|27 Jan 1991||0117||3.2|
|27 Jan 1991||0258||3.3|
|27 Jan 1991||1049||3.4|
|27 Jan 1991||1109||3.6|
|27 Jan 1991||2109||3.8|
Seismologists determined that the earthquakes were tectonic in origin and occurred at very shallow depth. No morphologic changes were noted at the volcano and fumarolic activity appeared to be similar to previous years. Seismic swarms had previously been recorded at Irazú in 1982 and 1987, although normal seismic activity is very low. Scientists noted that the shocks may be related to a fault SSE of the volcano, perhaps activated by the major earthquake [M 5.7] that occurred near Puriscal [50 km WSW] on 22 December.
Geological Summary. Irazú, one of Costa Rica's most active volcanoes, rises immediately E of the capital city of San José. The massive volcano covers an area of 500 km2 and is vegetated to within a few hundred meters of its broad flat-topped summit crater complex. At least 10 satellitic cones are located on its S flank. No lava flows have been identified since the eruption of the massive Cervantes lava flows from S-flank vents about 14,000 years ago, and all known Holocene eruptions have been explosive. The focus of eruptions at the summit crater complex has migrated to the W towards the historically active crater, which contains a small lake of variable size and color. Although eruptions may have occurred around the time of the Spanish conquest, the first well-documented historical eruption occurred in 1723, and frequent explosive eruptions have occurred since. Ashfall from the last major eruption during 1963-65 caused significant disruption to San José and surrounding areas.
Information Contacts: G. Soto and R. Barquero, ICE; Mario Fernández and Wilfredo Rojas, Escuela Centroamericana de Geología, Univ de Costa Rica.