Extensive lava flows, like those of Mount Merapi of Central Java, require thickness only of the order of meters and temperatures only slightly above the melting point to spread over distance of the order of hundreds of meters. Other things being equal the spreading distance is propotional to the cube of the thickness of the flow
The rheology and emplacement dynamics of basaltic and rhyolitic lava flows have been studied extensi...
Lava flows are not only a fascinating scientific problem, involving many branches of continuum mecha...
The dynamics of lava flow movement are controlled by the fluid interior. Crust, solids, and nondefor...
Extensive lava flows, like those of Mount Merapi of Central Java, require thickness only of the orde...
The Kaupulehu 1800-1801 lava flow of Hualalai volcano and the 1823 Keaiwa flow from the Great Crack ...
Because of their high eruption temperatures and ultrabasic composition, komatiite lavas had low visc...
Analysis of the formation of morphologically distinctive perched lava ponds produced in effusive bas...
We present a shallow, isothermal, Newtonian model for the transient interaction of lava flows with t...
Propagation of a lava flow is governed by slope topography, magma rheology, heat exchange with the a...
Propagation of a lava flow is governed by slope topography, magma rheology, heat exchange with the a...
Changes in the underlying slope of a lava flow impart a significant fraction of rotational energy be...
The dynamics of a lava flow is studied by a two-dimensional model describing a viscous fluid with Bi...
Because of their high eruption temperatures and ultrabasic composition, komatiite lavas had low visc...
none3We propose a model to describe lava tube formation, considering lava as a Newtonian fluid movin...
The prediction of lava flow advance and velocity is crucial during an effusive volcanic crisis. The ...
The rheology and emplacement dynamics of basaltic and rhyolitic lava flows have been studied extensi...
Lava flows are not only a fascinating scientific problem, involving many branches of continuum mecha...
The dynamics of lava flow movement are controlled by the fluid interior. Crust, solids, and nondefor...
Extensive lava flows, like those of Mount Merapi of Central Java, require thickness only of the orde...
The Kaupulehu 1800-1801 lava flow of Hualalai volcano and the 1823 Keaiwa flow from the Great Crack ...
Because of their high eruption temperatures and ultrabasic composition, komatiite lavas had low visc...
Analysis of the formation of morphologically distinctive perched lava ponds produced in effusive bas...
We present a shallow, isothermal, Newtonian model for the transient interaction of lava flows with t...
Propagation of a lava flow is governed by slope topography, magma rheology, heat exchange with the a...
Propagation of a lava flow is governed by slope topography, magma rheology, heat exchange with the a...
Changes in the underlying slope of a lava flow impart a significant fraction of rotational energy be...
The dynamics of a lava flow is studied by a two-dimensional model describing a viscous fluid with Bi...
Because of their high eruption temperatures and ultrabasic composition, komatiite lavas had low visc...
none3We propose a model to describe lava tube formation, considering lava as a Newtonian fluid movin...
The prediction of lava flow advance and velocity is crucial during an effusive volcanic crisis. The ...
The rheology and emplacement dynamics of basaltic and rhyolitic lava flows have been studied extensi...
Lava flows are not only a fascinating scientific problem, involving many branches of continuum mecha...
The dynamics of lava flow movement are controlled by the fluid interior. Crust, solids, and nondefor...
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