The volcano has been in moderate effusive activity for at least the past two weeks, feeding relatively small lava flows on the upper steep slope. A sudden increase in effusion rate seems to have caused the destabilization of the lava flows, generating rockfalls that turned into pyroclastic flows. The longest runout distance was reported as 2 km (INSIVUMEH). This is suggested by the appearance of strong tremor pulses the previous night.
In the meanwhile, explosive (strombolian) activity from the summit vent has remained weak.

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