Logo link to homepage

Report on Pavlof (United States) — 16 March-22 March 2022


Pavlof

Smithsonian / US Geological Survey Weekly Volcanic Activity Report,
16 March-22 March 2022
Managing Editor: Sally Kuhn Sennert

Please cite this report as:

Global Volcanism Program, 2022. Report on Pavlof (United States). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 16 March-22 March 2022. Smithsonian Institution and US Geological Survey.

Weekly Report (16 March-22 March 2022)

Pavlof

United States

55.417°N, 161.894°W; summit elev. 2493 m

All times are local (unless otherwise noted)


AVO reported that the eruption at a vent on Pavlof’s upper E flank was ongoing during 15-22 March, and seismic tremor persisted. Cloud cover sometimes prevented webcam and satellite views of the summit area, though almost-daily elevated surface temperatures identified in satellite images were consistent with minor lava effusion. Three small explosions were detected in local and regional infrasound data during 19-20 March. The Volcano Alert Level remained at Watch and the Aviation Color Code remained at Orange.

Geological Summary. The most active volcano of the Aleutian arc, Pavlof is a 2519-m-high Holocene stratovolcano that was constructed along a line of vents extending NE from the Emmons Lake caldera. Pavlof and its twin volcano to the NE, 2142-m-high Pavlof Sister, form a dramatic pair of symmetrical, glacier-covered stratovolcanoes that tower above Pavlof and Volcano bays. A third cone, Little Pavlof, is a smaller volcano on the SW flank of Pavlof volcano, near the rim of Emmons Lake caldera. Unlike Pavlof Sister, Pavlof has been frequently active in historical time, typically producing Strombolian to Vulcanian explosive eruptions from the summit vents and occasional lava flows. The active vents lie near the summit on the north and east sides. The largest historical eruption took place in 1911, at the end of a 5-year-long eruptive episode, when a fissure opened on the N flank, ejecting large blocks and issuing lava flows.

Source: US Geological Survey Alaska Volcano Observatory (AVO)