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Report on Sangay (Ecuador) — 2 February-8 February 2022


Sangay

Smithsonian / US Geological Survey Weekly Volcanic Activity Report,
2 February-8 February 2022
Managing Editor: Sally Kuhn Sennert

Please cite this report as:

Global Volcanism Program, 2022. Report on Sangay (Ecuador). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 2 February-8 February 2022. Smithsonian Institution and US Geological Survey.

Weekly Report (2 February-8 February 2022)

Sangay

Ecuador

2.005°S, 78.341°W; summit elev. 5286 m

All times are local (unless otherwise noted)


IG reported a high level of activity at Sangay during 2-7 February, and seismicity was characterized by daily explosions, long-period earthquakes, and signals indicating emissions. Weather clouds and rain often prevented visual and webcam observations of the volcano, though almost daily ash-and-gas plumes were identified in satellite images by the Washington VAAC or in webcam views; plumes rose as high as 1.5 km above the volcano and drifted in multiple directions. Multiple daily thermal anomalies over the volcano were visible in satellite data. Several ash emissions were observed in satellite images on 8February; at 0430 an ash plume rose more than 7 km above the summit, the highest a plume had risen since the current eruption started in 2019. Ashfall was reported in areas to the NW, in the provinces of Chimborazo and Bolivar.

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 horseshoe-shaped 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 sculpted by heavy rains into steep-walled canyons up to 600 m deep. The earliest report of a historical eruption was in 1628. More or less 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.

Source: Instituto Geofísico-Escuela Politécnica Nacional (IG)