Lava flows are gravity currents of partially molten rock that cool as they flow, in some cases
melting the surface over which they flow but in all cases gradually solidifying until they come …

Measurement of effusion rate is a primary objective for studies that model lava flow and
magma system dynamics, as well as for monitoring efforts during on-going eruptions …

The mid-ocean ridge (MOR) is the largest, most continuous volcanic system on Earth, yet we
have directly observed, mapped or sampled less than one percent of its total surface area …

When considering the rheology of a suspension the fundamental physical aspect to be
quantified is the redistribution of strain between the deformable matrix fraction of the …

Samples collected from a lava channel active at Kīlauea Volcano during May 1997 are used
to constrain rates of lava cooling and crystallization during early stages of flow. Lava erupted …

Factors which control lava flow length are still not fully understood. The assumption that flow
length as mainly influenced by viscosity was contested by Walker (1973) who proposed that …

The growth of lava domes can be either quiescent or violent, with transitions between styles
of behavior commonly occurring with little warning. Here we propose that the behavior …

Eruption of the Soufrière Hills Volcano on Montserrat allowed the detailed documentation of
a Pélean dome-forming eruption. Dome growth between November 1995 and March 1998 …

The results of recent laboratory experiments with wax extruded beneath relatively cold water
may be extrapolated to predict the surface morphology of submarine lavas as a function of …

The work outlined herein describes an evaluation of a new green solvent working as a drug
solubility enhancer made up of a eutectic system comprising mixtures of capric acid and …