Decompression experiments identify kinetic controls on explosive silicic eruptions [PDF]
Margaret T. Mangan +2 more
openalex +1 more source
Mass and energy budgets of explosive volcanic eruptions
Analysis of the frequency‐size relationship of explosive volcanic eruptions for the past 2000 years reveals that the time‐averaged eruptive mass flux of tephra from subaerial explosive eruptions is 3×104 kg s−1. This mass flux corresponds to a thermal energy release of 4×1010 W.
openaire +2 more sources
Residential building and occupant vulnerability to pyroclastic density currents in explosive eruptions [PDF]
Ruth Spence +5 more
openalex +1 more source
Potential atmospheric impact of the Toba Mega‐Eruption ∼71,000 years ago [PDF]
An ∼6‐year long period of volcanic sulfate recorded in the GISP2 ice core about 71,100 ± 5000 years ago may provide detailed information on the atmospheric and climatic impact of the Toba mega‐eruption. Deposition of these aerosols occur at the beginning
Mayewski, Paul A. +5 more
core +3 more sources
Multiple shallow level sill intrusions coupled with hydromagmatic explosive eruptions marked the initial phase of Ferrar large igneous province magmatism in northern Victoria Land, Antarctica [PDF]
L. Viereck-Goette +3 more
openalex +1 more source
The Campi Flegrei caldera (Italy) is among the most productive volcanoes of the Mediterranean area. However, the volcanic history preceding the VEI 7 Campanian Ignimbrite eruption (~40 ka) is still poorly constrained.
Giada Fernandez +5 more
doaj +1 more source
Upper-atmosphere Aerosols: Properties and Natural Cycles [PDF]
The middle atmosphere is rich in its variety of particulate matter, which ranges from meteorite debris, to sulfate aerosols, to polar stratospheric ice clouds. Volcanic eruptions strongly perturb the stratospheric sulfate (Junge) layer.
Turco, Richard P.
core +1 more source
Sulfur‐rich volcanic eruptions happen sporadically. If Stratospheric Aerosol Injection (SAI) were to be deployed, it is likely that explosive volcanic eruptions would happen during such a deployment.
I. Quaglia +4 more
doaj +1 more source
The Geological History of Deep-Sea Volcanoes: Biosphere, Hydrosphere, and Lithosphere Interactions [PDF]
The geological evolution of seamounts has distinct influence on their interactions with the ocean, their hydrology, geochemical fluxes, biology, resources, and geohazards.
Hubert Staudigel, David A. Clague
doaj
The effects of outgassing on the transition between effusive and explosive silicic eruptions [PDF]
W. Degruyter +3 more
openalex +1 more source

