Report on Momotombo (Nicaragua) — 2 December-8 December 2015
Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 2 December-8 December 2015
Managing Editor: Sally Kuhn Sennert
Please cite this report as:
Global Volcanism Program, 2015. Report on Momotombo (Nicaragua). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 2 December-8 December 2015. Smithsonian Institution and US Geological Survey.
12.422°N, 86.54°W; summit elev. 1297 m
All times are local (unless otherwise noted)
Based on satellite and webcam observations, and seismic data, the Washington VAAC reported that during 2-3 December ash plumes from Momotombo rose to an altitude of 2.4 km (8,000 ft) a.s.l. and drifted 90-225 km NW and WNW.
Geologic Background. Momotombo is a young, 1297-m-high stratovolcano that rises prominently above the NW shore of Lake Managua, forming one of Nicaragua's most familiar landmarks. Momotombo began growing about 4500 years ago at the SE end of the Marrabios Range and consists of a somma from an older edifice that is surmounted by a symmetrical younger cone with a 150 x 250 m wide summit crater. Young lava flows from Momotombo have flowed down the NW flank into the 4-km-wide Monte Galán caldera. The youthful cone of Momotombito forms a 391-m-high island offshore in Lake Managua. Momotombo has a long record of strombolian eruptions, punctuated by occasional larger explosive activity. The latest eruption, in 1905, produced a lava flow that traveled from the summit to the lower NE base. A small black plume was seen above the crater after an April 10, 1996 earthquake, but later observations noted no significant changes in the crater. A major geothermal field is located on the southern flank of the volcano.