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Report on Ubinas (Peru) — 13 January-19 January 2016


Ubinas

Smithsonian Institution / US Geological Survey
Weekly Volcanic Activity Report, 13 January-19 January 2016
Managing Editor: Sally Sennert.

Please cite this report as:

Global Volcanism Program, 2016. Report on Ubinas (Peru) (Sennert, S, ed.). Weekly Volcanic Activity Report, 13 January-19 January 2016. Smithsonian Institution and US Geological Survey.

Weekly Report (13 January-19 January 2016)

Ubinas

Peru

16.345°S, 70.8972°W; summit elev. 5608 m

All times are local (unless otherwise noted)


Instituto Geofísico del Perú (IGP) Observatorio Volcanológico del Sur (OVS) reported that during 12-18 January the seismic network at Ubinas recorded an increase in the number and magnitude of long-period earthquakes and a decrease in volcano-tectonic events. Thermal anomalies were detected on 13 and 15 January. At 0640 on 15 January a plume rose 500 m above the crater's base. At 1253 an explosion generated an ash plume that rose 3 km above the crater's base and drifted S and SW. The report noted that this was the first explosive event since 5 November 2015.

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.

Source: Instituto Geofísico del Perú (IGP)