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Report on Arenal (Costa Rica) — December 1982

Scientific Event Alert Network Bulletin, vol. 7, no. 12 (December 1982)
Managing Editor: Lindsay McClelland.

Arenal (Costa Rica) Lava flows remain active

Please cite this report as:

Global Volcanism Program, 1982. Report on Arenal (Costa Rica) (McClelland, L., ed.). Scientific Event Alert Network Bulletin, 7:12. Smithsonian Institution. https://doi.org/10.5479/si.GVP.SEAN198212-345033.

Volcano Profile |  Complete Bulletin


Costa Rica

10.463°N, 84.703°W; summit elev. 1670 m

All times are local (unless otherwise noted)

The lava flow that had advanced down the SW flank since January stopped in August. A new lava flow, the 39th since 1968, began descending the SW flank in August. In early September, the front of its main lobe stopped at an elevation of ~700 m, but another lobe continued to move SW until November. In mid-November, another new flow began advancing NW. On 18 November, its front had reached an elevation of ~1,300 m. Vapor emissions and gas explosions continued in the active crater.

Geologic Background. Conical Volcán Arenal is the youngest stratovolcano in Costa Rica and one of its most active. The 1670-m-high andesitic volcano towers above the eastern shores of Lake Arenal, which has been enlarged by a hydroelectric project. Arenal lies along a volcanic chain that has migrated to the NW from the late-Pleistocene Los Perdidos lava domes through the Pleistocene-to-Holocene Chato volcano, which contains a 500-m-wide, lake-filled summit crater. The earliest known eruptions of Arenal took place about 7000 years ago, and it was active concurrently with Cerro Chato until the activity of Chato ended about 3500 years ago. Growth of Arenal has been characterized by periodic major explosive eruptions at several-hundred-year intervals and periods of lava effusion that armor the cone. An eruptive period that began with a major explosive eruption in 1968 ended in December 2010; continuous explosive activity accompanied by slow lava effusion and the occasional emission of pyroclastic flows characterized the eruption from vents at the summit and on the upper western flank.

Information Contacts: J. Barquero H. and E. Malavassi R., Univ. Nacional, Heredia.