Slowly advancing lava flow from the vent and weak surface temperatures (image: Sentinel 2)
The effusive eruption at the volcano continues and is characterized by slow-paced viscous lava flow.
The slow rate of the lava caused its thickening around the vent rather than the length progress as detected in satellite-based radar observations.
An attached satellite image from yesterday shows weakly elevated temperatures near the effusive vent.
The steep terrain near the lava flow lobes may cause to detach of lava blocks from it and turn develop into rockfalls tumbling down the valleys.
The seismic activity continues at low levels.
Source: Alaska Volcano Observatory volcano activity update 16 July 2022