Report on Poas (Costa Rica) — October 1991

Bulletin of the Global Volcanism Network, vol. 16, no. 10 (October 1991)
Managing Editor: Lindsay McClelland

Poas (Costa Rica) Continued fumarolic activity; lake level drops

Please cite this report as:

Global Volcanism Program, 1991. Report on Poas (Costa Rica). In: McClelland, L (ed.), Bulletin of the Global Volcanism Network, 16:10. Smithsonian Institution. http://dx.doi.org/10.5479/si.GVP.BGVN199110-345040.

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Poas

Costa Rica

10.2°N, 84.233°W; summit elev. 2708 m

All times are local (unless otherwise noted)


Fumarolic activity in the yellowish-green crater lake continued through October, and mats of sulfur were observed floating on the water's surface. In September, strong bubbling was observed in the N- and NW-central parts of the lake, which was at 76.3°C with a pH <0.5. Lake measurements on 16 October indicated that the lake level had fallen 15 cm since 18 September, despite continued rains; water temperature was 74.4°C. Fumaroles on the 1953-55 dome ranged to 90.6°C in September and 88.4°C in October.

Geologic Background. The broad, well-vegetated edifice of Poás, one of the most active volcanoes of Costa Rica, contains three craters along a N-S line. The frequently visited multi-hued summit crater lakes of the basaltic-to-dacitic volcano, which is one of Costa Rica's most prominent natural landmarks, are easily accessible by vehicle from the nearby capital city of San José. A N-S-trending fissure cutting the 2708-m-high complex stratovolcano extends to the lower northern flank, where it has produced the Congo stratovolcano and several lake-filled maars. The southernmost of the two summit crater lakes, Botos, is cold and clear and last erupted about 7500 years ago. The more prominent geothermally heated northern lake, Laguna Caliente, is one of the world's most acidic natural lakes, with a pH of near zero. It has been the site of frequent phreatic and phreatomagmatic eruptions since the first historical eruption was reported in 1828. Eruptions often include geyser-like ejections of crater-lake water.

Information Contacts: R. Barquero and G. Soto, ICE.