Report on San Cristobal (Nicaragua) — April 1983
Scientific Event Alert Network Bulletin, vol. 8, no. 4 (April 1983)
Managing Editor: Lindsay McClelland.
San Cristobal (Nicaragua) Slow fumarole temperature increase; gas column
Please cite this report as:
Global Volcanism Program, 1983. Report on San Cristobal (Nicaragua). In: McClelland, L. (ed.), Scientific Event Alert Network Bulletin, 8:4. Smithsonian Institution. https://doi.org/10.5479/si.GVP.SEAN198304-344020.
12.702°N, 87.004°W; summit elev. 1745 m
All times are local (unless otherwise noted)
Temperatures continued to increase slowly, to 620°C on 2 February. A strong gas column was blown W. New N-S-trending fissures were observed. During February, 13-14 seismic events were recorded per day, but could only be detected by very sensitive instruments.
Geologic Background. The San Cristóbal volcanic complex, consisting of five principal volcanic edifices, forms the NW end of the Marrabios Range. The symmetrical 1745-m-high youngest cone, named San Cristóbal (also known as El Viejo), is Nicaragua's highest volcano and is capped by a 500 x 600 m wide crater. El Chonco, with several flank lava domes, is located 4 km W of San Cristóbal; it and the eroded Moyotepe volcano, 4 km NE of San Cristóbal, are of Pleistocene age. Volcán Casita, containing an elongated summit crater, lies immediately east of San Cristóbal and was the site of a catastrophic landslide and lahar in 1998. The Plio-Pleistocene La Pelona caldera is located at the eastern end of the complex. Historical eruptions from San Cristóbal, consisting of small-to-moderate explosive activity, have been reported since the 16th century. Some other 16th-century eruptions attributed to Casita volcano are uncertain and may pertain to other Marrabios Range volcanoes.
Information Contacts: D. Fajardo B., INETER.