Report on Tenorio (Costa Rica) — October 1997
Bulletin of the Global Volcanism Network, vol. 22, no. 10 (October 1997)
Managing Editor: Richard Wunderman.
Tenorio (Costa Rica) Small earthquake swarms near summit and SSW flank
Please cite this report as:
Global Volcanism Program, 1997. Report on Tenorio (Costa Rica) (Wunderman, R., ed.). Bulletin of the Global Volcanism Network, 22:10. Smithsonian Institution.
10.673°N, 85.015°W; summit elev. 1916 m
All times are local (unless otherwise noted)
During 5-27 October, 14 earthquakes were located on a 5-km-long SE-NW trend from the summit of Tenorio (figure 1). The swarm, centered around 10.7°N, 85.03°W, was possibly associated with known faults. The earthquakes had depths of 5-10 km and magnitudes of 0.6-2.1.
|Figure 1. Major faults in the Guanacaste Range of Costa Rica and October earthquake locations around Miravalles and Tenorio volcanoes. During 5-27 October, 620 earthquakes were recorded, but only 187 could be located. Courtesy of ICE.|
An unrelated swarm consisting of 27 events occurred during the same period near the village of Tierras Morenas at the SSW foot of Tenorio. The swarm was centered at 10.6°N, 85.0°W and was aligned along a 7-km NE-SW trend, possibly correlating to known faults. The earthquakes had depths of 7-12 km and magnitudes of 0.4-3.3.
Geologic Background. The 225 km2 dominantly andesitic Tenorio volcanic massif anchors the SE end of the Guanacaste Range and consists of a cluster of densely forested NNW-SSE-trending volcanic cones. Overlapping lava flows from the principal peak, Tenorio, blanket the NW-to-SW flanks and descend the NE flank. The NW-most of three craters of the central cone is sparsely vegetated and appears to be the most recently active. Volcán Montezuma to the north has twin craters, the northern of which fed a lava flow to the NE. Additional pyroclastic cones are found to the NE and SW of the central complex, and the Bijagua lava domes were constructed on the northern flank. A major debris avalanche covered about 100 km2 below the S flank. A legend exists of an eruption in 1816, but the volcano was densely forested at the time of an 1864 visit by Seebach and is not considered to have erupted in historical time. Fumarolic activity is present on the NE flank.
Information Contacts: Gerardo J. Soto and Waldo Taylor, Oficina de Sismología y Vulcanología, Departamento de Geología, Instituto Costarricense de Electricidad (ICE), Apartado 10032-1000, San José, Costa Rica.