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Report on Reventador (Ecuador) — 1 April-7 April 2015

Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 1 April-7 April 2015
Managing Editor: Sally Kuhn Sennert

Please cite this report as:

Global Volcanism Program, 2015. Report on Reventador (Ecuador). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 1 April-7 April 2015. Smithsonian Institution and US Geological Survey.

Volcano Profile |  Weekly Report (1 April-7 April 2015)


Reventador

Ecuador

0.077°S, 77.656°W; summit elev. 3562 m

All times are local (unless otherwise noted)


During 1-7 April IG reported moderate seismic activity including explosions, long-period earthquakes, harmonic tremor, and occasional tremor at Reventador; cloud cover often prevented visual observations. During 1-2 and 6 April incandescence from the crater and a lava flow on the SW flank were visible with the aid of an infrared camera. On 3 April a steam plume rose 600 m above the crater and drifted NW. The next day a steam-and-ash plume rose 500 m and drifted W. On 6 April a steam-and-ash plume rose 1 km and drifted NW.

Geologic Background. Reventador is the most frequently active of a chain of Ecuadorian volcanoes in the Cordillera Real, well east of the principal volcanic axis. The forested, dominantly andesitic Volcán El Reventador stratovolcano rises to 3562 m above the jungles of the western Amazon basin. A 4-km-wide caldera widely breached to the east was formed by edifice collapse and is partially filled by a young, unvegetated stratovolcano that rises about 1300 m above the caldera floor to a height comparable to the caldera rim. It has been the source of numerous lava flows as well as explosive eruptions that were visible from Quito in historical time. Frequent lahars in this region of heavy rainfall have constructed a debris plain on the eastern floor of the caldera. The largest historical eruption took place in 2002, producing a 17-km-high eruption column, pyroclastic flows that traveled up to 8 km, and lava flows from summit and flank vents.

Source: Instituto Geofísico-Escuela Politécnica Nacional (IG)