Report on Turrialba (Costa Rica) — December 1982
Scientific Event Alert Network Bulletin, vol. 7, no. 12 (December 1982)
Managing Editor: Lindsay McClelland.
Turrialba (Costa Rica) Activity level unchanged; no activity seen in the E crater
Please cite this report as:
Global Volcanism Program, 1982. Report on Turrialba (Costa Rica). In: McClelland, L (ed.), Scientific Event Alert Network Bulletin, 7:12. Smithsonian Institution. https://doi.org/10.5479/si.GVP.SEAN198212-345070.
10.025°N, 83.767°W; summit elev. 3340 m
All times are local (unless otherwise noted)
Activity remained the same as in previous years. The mean temperature was 86°C in the central crater and 89°C in the W crater. The E crater showed no activity.
Geologic Background. Turrialba, the easternmost of Costa Rica's Holocene volcanoes, is a large vegetated basaltic-to-dacitic stratovolcano located across a broad saddle NE of Irazú volcano overlooking the city of Cartago. The massive edifice covers an area of 500 km2. Three well-defined craters occur at the upper SW end of a broad 800 x 2200 m summit depression that is breached to the NE. Most activity originated from the summit vent complex, but two pyroclastic cones are located on the SW flank. Five major explosive eruptions have occurred during the past 3500 years. A series of explosive eruptions during the 19th century were sometimes accompanied by pyroclastic flows. Fumarolic activity continues at the central and SW summit craters.
Information Contacts: J. Barquero H., E. Malavassi R., Univ. Nacional, Heredia.