Dome-building eruptions may vary from unthreatening effusion to highly unpredictable and hazardous activity including collapse of domes and associated pyroclastic flow hazards. We analyse the influence of the thermal cooling and the crystal content growth on the lava dome morphology at Volcán de Colima in Mexico during a long dome-building episode lasting from early 2007 to fall 2009 without explosive dome destruction. For this, we develop several mathematical models of lava dome dynamics including the kinetics of crystal content growth, temperature-dependence of melt viscosity, latent heat, and nonlinear heat exchange between the lava and the air. Camera images of the lava dome growth together with...
International audienceDuring eruptive activity of andesitic stratovolcanoes, the extrusion of lava d...
The evolution of rhyolitic lava from effusion to cessation of activity is poorly understood. Recent...
Propagation of a lava flow is governed by slope topography, magma rheology, heat exchange with the a...
The growth of lava domes can be either quiescent or violent, with transitions between styles of beha...
Subduction zone volcanism occurs due to partial melting from subducting slabs, which generally resul...
Dome-forming volcanic eruptions typically involve the slow extrusion of viscous lava onto a steep-si...
Dome-forming eruption is a frequent eruptive style and a major hazard on numerous volcanoes worldwid...
Lava domes comprise core, carapace, and clastic talus components. They can grow endogenously by infl...
We investigate high-resolution digital photographs and infrared images of the lava dome eruption at ...
Lava domes arc formed during molten lava eruption. Various predictions of flow growth and eruption ...
The thermal boundary layer at the surface of a volcanic lava dome is investigated through a continuu...
International audienceThe most recent eruptive phase of Volc'an de Colima, Mexico, started in 1998 a...
International audienceIn December of 2017, a lava dome emerged at the Nevados de Chillan volcanic co...
We consider the process of slow extrusion of very viscous magma that forms lava domes. Dome-buildin...
Lava dome collapses can lead to explosive activity and pyroclastic flow generation which makes them ...
International audienceDuring eruptive activity of andesitic stratovolcanoes, the extrusion of lava d...
The evolution of rhyolitic lava from effusion to cessation of activity is poorly understood. Recent...
Propagation of a lava flow is governed by slope topography, magma rheology, heat exchange with the a...
The growth of lava domes can be either quiescent or violent, with transitions between styles of beha...
Subduction zone volcanism occurs due to partial melting from subducting slabs, which generally resul...
Dome-forming volcanic eruptions typically involve the slow extrusion of viscous lava onto a steep-si...
Dome-forming eruption is a frequent eruptive style and a major hazard on numerous volcanoes worldwid...
Lava domes comprise core, carapace, and clastic talus components. They can grow endogenously by infl...
We investigate high-resolution digital photographs and infrared images of the lava dome eruption at ...
Lava domes arc formed during molten lava eruption. Various predictions of flow growth and eruption ...
The thermal boundary layer at the surface of a volcanic lava dome is investigated through a continuu...
International audienceThe most recent eruptive phase of Volc'an de Colima, Mexico, started in 1998 a...
International audienceIn December of 2017, a lava dome emerged at the Nevados de Chillan volcanic co...
We consider the process of slow extrusion of very viscous magma that forms lava domes. Dome-buildin...
Lava dome collapses can lead to explosive activity and pyroclastic flow generation which makes them ...
International audienceDuring eruptive activity of andesitic stratovolcanoes, the extrusion of lava d...
The evolution of rhyolitic lava from effusion to cessation of activity is poorly understood. Recent...
Propagation of a lava flow is governed by slope topography, magma rheology, heat exchange with the a...