Report on Sangay (Ecuador) — 9 October-15 October 2024
Smithsonian Institution / US Geological Survey
Weekly Volcanic Activity Report, 9 October-15 October 2024
Managing Editor: Sally Sennert.
Please cite this report as:
Global Volcanism Program, 2024. Report on Sangay (Ecuador) (Sennert, S, ed.). Weekly Volcanic Activity Report, 9 October-15 October 2024. Smithsonian Institution and US Geological Survey.
Sangay
Ecuador
2.005°S, 78.341°W; summit elev. 5286 m
All times are local (unless otherwise noted)
The Instituto Geofísico-Escuela Politécnica Nacional (IG-EPN) reported that high levels of eruptive activity continued at Sangay during 8-15 October. The seismic network recorded 102-249 daily explosions during 8-12 October; there were no counts during the rest of the week due to data transmission problems. Gas-and-ash plumes visible in webcam and/or satellite images on most days rose as high as 1.6 km above the summit and drifted mainly W, WSW, and SW and occasionally to the NE. Weather conditions often obscured views, though several episodes of crater incandescence were observed during dark hours and incandescent material descended the SE drainage as far as 2 km. Secretaría de Gestión de Riesgos (SGR) maintained the Alert Level at Yellow (the second highest level on a four-color scale).
Geological Summary. The isolated Sangay volcano, located east of the Andean crest, is the southernmost of Ecuador's volcanoes and its most active. The steep-sided, glacier-covered, dominantly andesitic volcano grew within the open calderas of two previous edifices which were destroyed by collapse to the east, producing large debris avalanches that reached the Amazonian lowlands. The modern edifice dates back to at least 14,000 years ago. It towers above the tropical jungle on the east side; on the other sides flat plains of ash have been eroded by heavy rains into steep-walled canyons up to 600 m deep. The earliest report of an eruption was in 1628. Almost continuous eruptions were reported from 1728 until 1916, and again from 1934 to the present. The almost constant activity has caused frequent changes to the morphology of the summit crater complex.
Sources: Instituto Geofísico-Escuela Politécnica Nacional (IG-EPN), Secretaría de Gestión de Riesgos (SGR)