Three-dimensional magnetotelluric modeling of Vulcano Island (Eolie, Italy) and its implications for understanding recent volcanic unrest. [PDF]
Sci Rep, 2023 Di Giuseppe MG, Isaia R, Troiano A.
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Seismic background level (SBL) growth can reveal slowly developing long-term eruption precursors. [PDF]
Sci Rep, 2023 Ichihara M +5 more
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Volcanological constraints of Archaean tectonics [PDF]
Volcanological and trace element geochemical data can be integrated to place some constraints upon the size, character and evolutionary history of Archean volcanic plumbing, and hence indirectly, Archean tectonics.
Ayres, L. D., Thurston, P. C.
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Revista Politécnica, 2014 El volcán Tungurahua desde su reactivación en 1999 ha alternado fases de elevada actividad volcánica, caracterizada por fuertes emisiones de gas y ceniza, explosiones tipo cañón y episodios de fuente de lava, así como también con fases de baja actividad ...
Jorge Eduardo Bustillos +6 more
doaj
Recent volcanic activity at the Asama volcano and long-period seismic signals. [PDF]
Proc Jpn Acad Ser B Phys Biol Sci, 2022 Takeo M, Aoki Y, Koyama T.
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Bubble-enhanced basanite-tephrite mixing in the early stages of the Cumbre Vieja 2021 eruption, La Palma, Canary Islands. [PDF]
Sci Rep, 2023 González-García D +3 more
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An investigation of volcanic depressions. Part 1 - Geologic and geophysical features of calderas Progress report [PDF]
Preferred classification of calderas and volcano- tectonic depressions based on relative amounts of lava and proclastic ...
Mc Birney, A. R., Williams, H.
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Volcanic Vortex Rings: Axial Dynamics, Acoustic Features, and Their Link to Vent Diameter and Supersonic Jet Flow. [PDF]
Geophys Res Lett, 2021 Taddeucci J +8 more
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Eruption dynamics of cyclic vulcanian explosions from Galeras volcano, Colombia
, 2019 Extended periods of volcanic unrest characterised by repeated, or cyclical, vulcanian explosions are common at arc volcanoes worldwide. Such explosions are thought to occur following the emplacement of a dense, degassed, lowper-meability plug of highly crystalline and highly viscous magma in the shallow conduit. Despite advances in the understanding of
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