Report on Arenal (Costa Rica) — July 1989
Scientific Event Alert Network Bulletin, vol. 14, no. 7 (July 1989)
Managing Editor: Lindsay McClelland.
Arenal (Costa Rica) Strombolian activity and seismicity increase; lava flow
Please cite this report as:
Global Volcanism Program, 1989. Report on Arenal (Costa Rica). In: McClelland, L. (ed.), Scientific Event Alert Network Bulletin, 14:7. Smithsonian Institution. https://doi.org/10.5479/si.GVP.SEAN198907-345033.
10.463°N, 84.703°W; summit elev. 1670 m
All times are local (unless otherwise noted)
The number of volcanic earthquakes at Arenal recorded by the Red Sismológica Nacional increased on 20 July, to a daily mean of 19 for the rest of the month. Seismicity was most frequent on the 26th, when 30 events were recorded. A moderate increase in Strombolian activity was associated with the enhanced seismicity. A small lava flow descended the NW flank during July.
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: R. Barquero and G. Alvarado, ICE; G. Soto, Univ de Costa Rica.