During the last week of May, there was an increase in the number of long-period earthquakes at Reventador associated with a new lava flow. A lava flow emitted previously continued to travel SE towards the Marquer and Montana rivers. During 2-3 June, incandescence was visible in the crater. On 6 June ash-and-gas plumes were emitted from the volcano.

Geological Summary. Volcán El 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 stratovolcano has 4-km-wide avalanche scarp open to the E formed by edifice collapse. A young, unvegetated, cone rises from the amphitheater floor about 1,300 m to a height comparable to the rim. It has been the source of numerous lava flows as well as explosive eruptions visible from Quito, about 90 km ESE. Frequent lahars in this region of heavy rainfall have constructed a debris plain on the eastern floor of the scarp. The largest recorded 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: Washington Volcanic Ash Advisory Center (VAAC)