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Report on Las Pilas (Nicaragua) — February 1991

Bulletin of the Global Volcanism Network, vol. 16, no. 2 (February 1991)
Managing Editor: Lindsay McClelland.

Las Pilas (Nicaragua) Continued fumarolic activity; many young prehistoric lava flows

Please cite this report as:

Global Volcanism Program, 1991. Report on Las Pilas (Nicaragua). In: McClelland, L. (ed.), Bulletin of the Global Volcanism Network, 16:2. Smithsonian Institution. https://doi.org/10.5479/si.GVP.BGVN199102-344080.

Volcano Profile |  Complete Bulletin


Las Pilas

Nicaragua

12.495°N, 86.688°W; summit elev. 1088 m

All times are local (unless otherwise noted)


"The El Hoyo fumarole was visited 3 times (15:04) and showed no discernable change from wet- to dry-season conditions (98°C). There is no other strong thermal activity in the summit region of El Hoyo.

"The central crater walls of El Hoyo (150 m deep) are composed of lava and agglutinated spatter, probably produced by Hawaiian activity (figure 1). In contrast, Las Pilas, Asososca, and Cerro Negro are predominantly scoria cones formed by Strombolian eruptions. All vents have produced extensive lava flows. Poorly vegetated flows extend up to 15 km from both Las Pilas and El Hoyo and are probably less than a few thousand years old."

Figure (see Caption) Figure 1. Sketch map of the El Hoyo volcanic complex and Cerro Negro. After Bice (1980).

Reference. Bice, D.C., 1980, Tephra stratigraphy and physical aspects of recent volcanism near Managua, Nicaragua: Ph.D. Dissertation, Univ of California, Berkeley, 422 p.

Geologic Background. Las Pilas volcanic complex, overlooking Cerro Negro volcano to the NW, includes a diverse cluster of cones around the central vent, Las Pilas (El Hoyo). A N-S-trending fracture system cutting across the edifice is marked by numerous well-preserved flank vents, including maars, that are part of a 30-km-long volcanic massif. The Cerro Negro chain of cinder cones is listed separately in this compilation because of its extensive historical eruptions. The lake-filled Asososca maar is located adjacent to the Cerro Asososca cone on the southern side of the fissure system, south of the axis of the Marrabios Range. Two small maars west of Lake Managua are located at the southern end of the fissure. Aside from a possible eruption in the 16th century, the only historical eruptions of Las Pilas took place in the 1950s from a fissure that cuts the eastern side of the 700-m-wide summit crater and extends down the N flank.

Information Contacts: B. van Wyk de Vries, O. Castellón, A. Murales, and V. Tenorio, INETER.