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7:47 PM · Dec 8, 2022

USGS (12.8.22) - The Northeast Rift Zone eruption of Mauna Loa continues with a major change overnight. The fissure 3 (F3) vent continues to erupt but the supply of lava appears to be much reduced this morning. Lava is overtopping channels near the vent with flows extending no farther than 2.5 mi (4 km) from the vent. The channels below this point appear drained of lava and probably no longer feed the main flow front. As of 5:30 a.m. today, December 8, the flow front was stalled about 1.7 mi (2.8 km) from the Daniel K. Inouye Highway (Saddle Road). The lava flow is now inactive for most of its lower length, but the flow front may appear to advance a little as it settles. Sulfur dioxide (SO2) emission rates of approximately 120,000 tonnes per day (t/d) were measured on December 4, 2022, and remain elevated at this time. Volcanic gas is rising high and vertically into the atmosphere before being blown to the west at high altitude, generating vog (volcanic air pollution) in areas downwind. The Hawaii Interagency Vog Information Dashboard has detailed information about vog: Forecasts for the dispersion of vog can be found on the VMAP Vog Forecast Dashboard: Tremor (a signal associated with subsurface fluid movement) continues beneath the currently active fissure. This indicates that magma is still being supplied to the fissure, and activity is likely to continue as long as we see this signal. There is no active lava within Moku'āweoweo caldera nor the Southwest Rift Zone. We do not expect any eruptive activity outside the Northeast Rift Zone. ---- END OF USGS UPDATE ---- Timelapse of increased fountaining last night:

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