Research news on eruption cloud

An eruption cloud is a transient, three-dimensional mass of gas, ash, and entrained ambient air generated above a volcanic vent during explosive activity, characterized by vigorous convective ascent and turbulent mixing. It typically develops when magma fragmentation produces pyroclasts and volatiles at high mass flux, driving a buoyant column that can transition from a jet-dominated region near the vent to a convective plume and, at neutral buoyancy, an umbrella region spreading laterally. Eruption clouds exhibit complex microphysical processes, including ash aggregation, ice formation, and electrostatic charging, and they play a central role in tephra dispersal, atmospheric loading of volcanic aerosols, and associated hazards to aviation and climate.

Ever-restless Mount Dukono erupts

The volcano on Indonesia's Halmahera Island routinely ejects ash, volcanic gases, and volcanic bombs. In May 2026, the Global Volcanism Program reported nine actively erupting volcanoes in Indonesia—more than any other country ...

Hayli Gubbi's explosive first impression

On November 23, 2025, the Hayli Gubbi volcano in northern Ethiopia erupted in dramatic fashion. The shield volcano in the Danakil (or Afar) Depression began spewing ash and volcanic gases at around 11:30 a.m. local time (8:30 ...

Eruption of long-dormant Ethiopian volcano subsides

Volcanic activity in northern Ethiopia's long-dormant Hayli Gubbi volcano subsided Tuesday, days after an eruption that left a trail of destruction in nearby villages and caused flight cancellations after ash plumes disrupted ...

Ethiopian volcanic plume captured by satellite

The Hayli Gubbi volcano in northeast Ethiopia, believed to have been dormant for up to 12,000 years, erupted on 23 November 2025, sending a massive plume of ash and sulfur dioxide high into the atmosphere.

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