Author Posting. © Cambridge University Press, 2000. This article is posted here by permission of Cambridge University Press for personal use, not for redistribution. The definitive version was published in Journal of Fluid Mechanics 403 (2000): 37-65, doi:10.1017/S0022112099006916.The dynamics of expanding domes of isothermal lava are studied by treating the lava as a viscoplastic material with the Herschel–Bulkley constitutive law. Thin-layer theory is developed for radially symmetric extrusions onto horizontal plates. This provides an evolution equation for the thickness of the fluid that can be used to model expanding isothermal lava domes. Numerical and analytical solutions are derived that explore the effects of yield stress, shear t...
In planetary sciences, the emplacement of lava flows is commonly modelled using a single rheologica...
Surface structures on 'a'ā and blocky lavas reflect the internal flow dynamics during emplacement an...
Dome-forming eruption is a frequent eruptive style and a major hazard on numerous volcanoes worldwid...
This thesis is concerned with the spreading of a large mass of fluid under the influence of gravity ...
The transition from an endogenous to an exogenous regime of lava dome growth must be achieved by the...
Modeling volcanic phenomena is complicated by free-surfaces often supporting large rheological gradi...
none3We propose a model to describe lava tube formation, considering lava as a Newtonian fluid movin...
At least two instabilities have been identified and utilized in lava flow studies: surface folding a...
The growth of lava domes can be either quiescent or violent, with transitions between styles of beha...
none2noThe dynamics of a lava flow is studied by a two-dimensional model describing a viscous fluid ...
We propose a model to describe lava tube formation, considering lava as a Newtonian fluid moving dow...
Research suggests that variations in lava dome morphology on different planets will depend much more...
Lava domes form when a highly viscous magma erupts on the surface. Several types of lava dome morpho...
In planetary sciences, the emplacement of lava flows is commonly modelled using a single rheological...
[1] The influence of a viscoplastic lava rheology on the dynamics of channeled lava flows is analyze...
In planetary sciences, the emplacement of lava flows is commonly modelled using a single rheologica...
Surface structures on 'a'ā and blocky lavas reflect the internal flow dynamics during emplacement an...
Dome-forming eruption is a frequent eruptive style and a major hazard on numerous volcanoes worldwid...
This thesis is concerned with the spreading of a large mass of fluid under the influence of gravity ...
The transition from an endogenous to an exogenous regime of lava dome growth must be achieved by the...
Modeling volcanic phenomena is complicated by free-surfaces often supporting large rheological gradi...
none3We propose a model to describe lava tube formation, considering lava as a Newtonian fluid movin...
At least two instabilities have been identified and utilized in lava flow studies: surface folding a...
The growth of lava domes can be either quiescent or violent, with transitions between styles of beha...
none2noThe dynamics of a lava flow is studied by a two-dimensional model describing a viscous fluid ...
We propose a model to describe lava tube formation, considering lava as a Newtonian fluid moving dow...
Research suggests that variations in lava dome morphology on different planets will depend much more...
Lava domes form when a highly viscous magma erupts on the surface. Several types of lava dome morpho...
In planetary sciences, the emplacement of lava flows is commonly modelled using a single rheological...
[1] The influence of a viscoplastic lava rheology on the dynamics of channeled lava flows is analyze...
In planetary sciences, the emplacement of lava flows is commonly modelled using a single rheologica...
Surface structures on 'a'ā and blocky lavas reflect the internal flow dynamics during emplacement an...
Dome-forming eruption is a frequent eruptive style and a major hazard on numerous volcanoes worldwid...