Results 61 to 70 of about 418,217 (192)
Venus: A Thick Basal Magma Ocean May Exist Today
Basal magma oceans develop in Earth and Venus after accretion as their mantles solidify from the middle outward. Fractional crystallization of the basal mantle is buffered by the core and radiogenic and latent heat in the magma ocean.
J. G. O'Rourke
doaj +1 more source
Modeling the Intermittent Lava Lake Drops Occurring Between 2015 and 2021 at Nyiragongo Volcano
Between 2015 and 2021, Nyiragongo's lava lake level experienced a linear increase punctuated by fast intermittent drops. These drops occurred synchronously to seismic swarm at approximately 15 km below the surface and extending laterally NE from the ...
D. Walwer +5 more
doaj +1 more source
The Tierra Blanca (TB) eruptive suite comprises the last four major eruptions of Ilopango caldera in El Salvador (≤45 ka), including the youngest Tierra Blanca Joven eruption (TBJ; ∼106 km3): the most voluminous event during the Holocene in Central ...
A. Cisneros de León +11 more
doaj +1 more source
Melt re-injection into large magma reservoir after giant caldera eruption at Kikai Caldera Volcano
Melt re-injection after a giant caldera eruption was quantitatively investigated for the Kikai Caldera Volcano in Japan, which erupted 7300 years ago (Kikai-Akahoya eruption). Our seismic refraction survey revealed a low-velocity anomaly directly beneath
Akihiro Nagaya +5 more
doaj +1 more source
Evolution of a silicic magma reservoir in the upper crust : Reyðarártindur pluton, Southeast Iceland
Field observations of extinct and exposed magma reservoirs shed light on processes operating in the roots of presently active volcanoes. The Reyðarártindur pluton, Southeast Iceland is an example of a fossil shallow magma reservoir that fed eruptions ...
Rhodes, Emma
core +1 more source
The interplay between melt, crystals, and volatile bubbles controls the physical properties of magmas in Earth's crust, the rate of phase separation, and, by extension, chemical differentiation. The mechanical processes that couple crystals, bubbles, and melt are nonlinear, and their expression in magmatic systems can vary greatly with the relative ...
Christian Huber +7 more
openaire +2 more sources
Probing Magma Reservoirs to Improve Volcano Forecasts
The roots of volcanoes remain enigmatic, largely because geophysical and petrological models remain rudimentary. Scientific drilling and exploration can help.
Jacob Lowenstern +2 more
openaire +1 more source
Modeling of Eruption Intervals and Durations by a Simple Magma System: the RC Magma System Model [PDF]
Eruption intervals and durations are controlled by various parameters of subsurface magma system including sizes of magma reservoirs and conduits, viscosity of magma, and magma supply rates. For the purpose of examining the effects of these parameters on
Motoo,UKAWA, 鵜川,元雄
core
Volcanic unrest as seen from the magmatic source: Reyðarártindur pluton, Iceland
How the Earth’s crust accommodates magma emplacement influences the signals that can be detected by monitoring volcano seismicity and surface deformation, which are routinely used to forecast volcanic eruptions.
Emma Rhodes +7 more
doaj +1 more source
Maars to calderas: end-members on a spectrum of explosive volcanic depressions
We discuss maar-diatremes and calderas as end-members on a spectrum of negative volcanic landforms (depressions) produced by explosive eruptions (note – we focus on calderas formed during explosive eruptions, recognizing that some caldera types are not ...
Danilo M. Palladino +3 more
doaj +1 more source

