Based on a significant meteorological notice (SIGMET), the Buenos Aires VAAC reported that an ash plume from Ubinas rose to altitudes of 5.5-7 km (26,000-27,000 ft) a.s.l. on 10 April and drifted W. INGEMMET reported that on 11 April, emissions of gas and ash produced plumes to altitudes of 6.2-6.4 km (20,000-21,000 ft) a.s.l. and drifted E. Based on an additional SIGMET, the Buenos Aires VAAC reported that an ash plume rose to altitudes of 6.1-6.4 km (20,000-21,000 ft) a.s.l. and drifted SE.

Geological Summary. The truncated appearance of Ubinas, Perú's most active volcano, is a result of a 1.4-km-wide crater at the summit. It is the northernmost of three young volcanoes located along a regional structural lineament about 50 km behind the main volcanic front. The growth and destruction of Ubinas I was followed by construction of Ubinas II beginning in the mid-Pleistocene. The upper slopes of the andesitic-to-rhyolitic Ubinas II stratovolcano are composed primarily of andesitic and trachyandesitic lava flows and steepen to nearly 45°. The steep-walled, 150-m-deep summit crater contains an ash cone with a 500-m-wide funnel-shaped vent that is 200 m deep. Debris-avalanche deposits from the collapse of the SE flank about 3,700 years ago extend 10 km from the volcano. Widespread Plinian pumice-fall deposits include one from about 1,000 years ago. Holocene lava flows are visible on the flanks, but activity documented since the 16th century has consisted of intermittent minor-to-moderate explosive eruptions.

Sources: Buenos Aires Volcanic Ash Advisory Center (VAAC), Instituto Geológico Minero y Metalúrgico (INGEMMET)