Results 101 to 110 of about 2,889,255 (157)

Enhanced crystal-melt segregation within dynamic mush systems links silicic cumulates with caldera-forming eruptions. [PDF]

Nat Commun
Lino LM, Quiroz-Valle FR, Vlach SRF, Bachmann O, Jerram DA, Janasi VA, Hueck M, Macêdo Filho AA, Basei MÂS.   +8 more
europepmc   +1 more source

High-resolution topography reveals morphological changes of Stromboli volcano following the July 2024 eruption. [PDF]

Sci Data
Civico R, Ricci T, Cecili A, Scarlato P.
europepmc   +1 more source

Precipitation induced by explosive volcanism on Mars and its implications for unexpected equatorial ice. [PDF]

Nat Commun
Hamid SS, Kerber L, Clarke AB.
europepmc   +1 more source

Long-term reduced lunar mantle revealed by Chang'e-5 basalt. [PDF]

Nat Commun
Zhang H, Yang W, Zhang D, Tian H, Ruan R, Hu S, Chen Y, Hui H, Lin Y, Mitchell RN, Zhang D, Wu S, Jia L, Gu L, Lin Y, Li X, Wu F.   +16 more
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Tephra fall probabilistic hazard maps for VEI 3 and VEI 4 eruptions at Mt. Garibaldi (<i>Nch'</i> <i>k</i> <i>ay')</i> volcano, British Columbia, Canada. [PDF]

J Appl Volcanol
Osman S, Jones TJ, Le Moigne Y, Kelman M.   +3 more
europepmc   +1 more source

Evidence that the Aso-3 caldera-forming eruption (southwest Japan) marks the termination of Marine Isotope Stage (MIS) 6.

Quat Sci Rev
McLean D, Albert PG, Jones G, Staff RA, Francke A, Vineberg SO, Tyler JJ, Saito-Kato M, Sagawa T, Kaneko K, Buckland H, Suzuki T, Kimura JI, Chang Q, Hoshizumi H, Miyabuchi Y, Manning CJ, Yamada K, Kitaba I, Ikehara K, SG14 Project Members, Nakagawa T, Smith VC.   +22 more
europepmc   +1 more source

Characterising pyroclastic density current grainsize data

Engwell, Samantha, Calder, Eliza, Breard, Eric   +2 more
openaire   +1 more source

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A Fast, Calibrated Model for Pyroclastic Density Currents Kinematics and Hazard

Journal of Volcanology and Geothermal Research, 2016
Abstract Multiphase flow models represent valuable tools for the study of the complex, non-equilibrium dynamics of pyroclastic density currents. Particle sedimentation, flow stratification and rheological changes, depending on the flow regime, interaction with topographic obstacles, turbulent air entrainment, buoyancy reversal, and other complex ...
Tomaso Esposti Ongaro, Fulvio Cornolti
exaly   +3 more sources