Deep Magma Transport Control on the Size and Evolution of Explosive Volcanic Eruptions
Explosive eruptions are the surface manifestation of dynamics that involve transfer of magma from the underground regions of magma accumulation. Evidence of the involvement of compositionally different magmas from different reservoirs is continuously ...
Simone Colucci, Paolo Papale
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Understanding the plume dynamics of explosive super-eruptions [PDF]
AbstractExplosive super-eruptions can erupt up to thousands of km3 of magma with extremely high mass flow rates (MFR). The plume dynamics of these super-eruptions are still poorly understood. To understand the processes operating in these plumes we used a fluid-dynamical model to simulate what happens at a range of MFR, from values generating intense ...
Antonio Costa +2 more
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Temporal variations of magma composition, eruption style and rate at Fuji Volcano, Japan
Mt. Fuji is an active basaltic volcano near the Tokyo metropolitan area; future eruptions could thus have serious nationwide impacts. To better understand recent volcanism at Fuji Volcano, we here clarify temporal variations of eruption rate and magma ...
Takahiro Yamamoto +2 more
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Atmospheric impact of the 1783-1784 Laki eruption: Part I Chemistry modelling. [PDF]
Results from the first chemistry-transport model study of the impact of the 1783–1784 Laki fissure eruption (Iceland: 64°N, 17°W) upon atmospheric composition are presented.
Stevenson, D. S.; id_orcid +17 more
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Volcanological challenges to understanding explosive large-scale eruptions
An explosive eruption, associated with the formation of a large ignimbrite sheet and collapsed caldera, is the most severe volcanic disaster on Earth.
Nobuo Geshi
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Explosive Behavior of Intermediate Magmas: The Example of Cotopaxi Volcano (Ecuador)
The variability in intensity and style shown by explosive volcanism has been traditionally explained by a complex interplay among melt composition and pre‐eruptive volatile content, which modulate magma ascent and conduit dynamics. However, magmas having
M. Pistolesi +5 more
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Sulfur as a binding agent of aggregates in explosive eruptions [PDF]
Understanding the mechanisms that govern ash aggregation is of critical importance in volcanology. Aggregation reduces the residence time of ash (≤2 mm) in the atmosphere strongly, by enhancing the sedimentation of finer-grained material generated during explosive eruptions.
Teresa Scolamacchia, Donald B. Dingwell
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High-latitude eruptions cast shadow over the African monsoon and the flow of the Nile [PDF]
Nile River records indicate very low flow following the 1783–1784 Laki volcanic eruption, as well as after other high-latitude volcanic eruptions. As shown by climate model simulations of the Laki eruption, significant cooling (−1° to −3°C) of the ...
Robock, A. +3 more
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Magma reservoir growth and ground deformation preceding the 79 CE Plinian eruption of Vesuvius
The 79 CE eruption of Vesuvius is the first documented Plinian eruption, also famous for the archaeological ruins of Pompeii and Herculaneum. Although much is known regarding the eruption dynamics and magma reservoir, little is known about the reservoir ...
Domenico M. Doronzo +7 more
doaj +1 more source
The origin of pelletal lapilli in explosive kimberlite eruptions [PDF]
Kimberlites are volatile-rich magmas from mantle depths of ≥ 150 km and are the primary source of diamonds. Kimberlite volcanism involves the formation of diverging pipes or diatremes, which are the locus of high-intensity explosive eruptions. A conspicuous and previously enigmatic feature of diatreme fills are 'pelletal lapilli'--well-rounded clasts ...
Gernon, Thomas M. +3 more
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