Ash emission in explosive silicic eruptions can have widespread impacts for human health, agriculture, infrastructure, and aviation. Estimates of the total grainsize distribution (TGSD) generated during explosive magma fragmentation underpins eruption models and ash dispersal forecasts. Conventionally, the TGSD constrained via erupted deposits is assumed to match the TGSD produced at explosive fragmentation. Here we present observations from within the vent of a recent rhyolitic eruption (Cordón Caulle, Chile, 2011–2012), demonstrating that fine (<63 μm diameter) and ultra-fine (<2.5 μm diameter) ash particles are captured and sintered to fracture surfaces, and thus sequestered in the shallow subsurface, rather than emitted. We establish a ...
The impact of explosive volcanic plumes on climate and on air traffic strongly depends on the concen...
Most volcanic ash particles with diameters <63 μm settle from eruption clouds as particle aggregates...
Explosive volcanic eruptions can eject large quantities of tephra into the atmosphere that can be di...
Ash emission in explosive silicic eruptions can have widespread impacts for human health, agricultur...
Tephra deposits result from explosive volcanic eruption and serve as indirect probes into fragmentat...
Tephra deposits result from explosive volcanic eruption and serve as indirect probes into fragmentat...
Explosive volcanic eruptions emit large proportions of very fine ash (\u3c30 μm) into the atmosphere...
Volcanic eruptions can produce ash particles with a range of sizes and morphologies. Here we morphol...
Some of the most complex volcanic thermodynamic processes occur when erupting magma interacts with w...
Volcanic ash particle properties depend upon their genetic fragmentation processes. Here, we introdu...
The size distribution of the population of particles injected into the atmosphere during a volcanic ...
Open conduit volcanoes are characterized by frequent, small scale explosive eruptions, which have a ...
Numerical modeling of ash plume dispersal is an important tool for forecasting and mitigating potent...
The size distribution of the population of particles injected into the atmosphere during a volcanic ...
The impact of explosive volcanic plumes on climate and on air traffic strongly depends on the concen...
Most volcanic ash particles with diameters <63 μm settle from eruption clouds as particle aggregates...
Explosive volcanic eruptions can eject large quantities of tephra into the atmosphere that can be di...
Ash emission in explosive silicic eruptions can have widespread impacts for human health, agricultur...
Tephra deposits result from explosive volcanic eruption and serve as indirect probes into fragmentat...
Tephra deposits result from explosive volcanic eruption and serve as indirect probes into fragmentat...
Explosive volcanic eruptions emit large proportions of very fine ash (\u3c30 μm) into the atmosphere...
Volcanic eruptions can produce ash particles with a range of sizes and morphologies. Here we morphol...
Some of the most complex volcanic thermodynamic processes occur when erupting magma interacts with w...
Volcanic ash particle properties depend upon their genetic fragmentation processes. Here, we introdu...
The size distribution of the population of particles injected into the atmosphere during a volcanic ...
Open conduit volcanoes are characterized by frequent, small scale explosive eruptions, which have a ...
Numerical modeling of ash plume dispersal is an important tool for forecasting and mitigating potent...
The size distribution of the population of particles injected into the atmosphere during a volcanic ...
The impact of explosive volcanic plumes on climate and on air traffic strongly depends on the concen...
Most volcanic ash particles with diameters <63 μm settle from eruption clouds as particle aggregates...
Explosive volcanic eruptions can eject large quantities of tephra into the atmosphere that can be di...