IG reported that moderate eruptive activity continued at Cotopaxi during 6-13 June. Seismic activity was mainly characterized by long-period earthquakes and tremors associated with daily emissions; one volcano-tectonic event was recorded during 6-7 June. Small gas-and-steam emissions rose as high as 300 m above the crater rim during 6-9 June. A small lahar was detected by the seismic network on 8 June and descended the NW flank. Several daily ash-and-gas emissions were visible during 10-13 June and were continuous during part of 12 June. The plumes rose 200-600 m above the crater rim and drifted NW, W, and SW. Servicio Nacional de Gestión de Riesgos y Emergencias (SNGRE) maintained the Alert Level at Yellow (the second lowest level on a four-color scale).

Geological Summary. The symmetrical, glacier-covered, Cotopaxi stratovolcano is Ecuador's most well-known volcano and one of its most active. The steep-sided cone is capped by nested summit craters, the largest of which is about 550 x 800 m in diameter. Deep valleys scoured by lahars radiate from the summit of the andesitic volcano, and large andesitic lava flows extend to its base. The modern edifice has been constructed since a major collapse sometime prior to about 5,000 years ago. Pyroclastic flows (often confused in historical accounts with lava flows) have accompanied many explosive eruptions, and lahars have frequently devastated adjacent valleys. Strong eruptions took place in 1744, 1768, and 1877. Pyroclastic flows descended all sides of the volcano in 1877, and lahars traveled more than 100 km into the Pacific Ocean and western Amazon basin. Smaller eruptions have been frequent since that time.

Sources: Instituto Geofísico-Escuela Politécnica Nacional (IG-EPN), Servicio Nacional de Gestión de Riesgos y Emergencias (SNGRE)