Forecasting the evolution of the 2021 Tajogaite eruption, La Palma, with TROPOMI/PlumeTraj-derived SO<sub>2</sub> emission rates. [PDF]
Esse B +7 more
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Biomonitoring of Inorganic Pollutants in Blood Samples of Population Affected by the Tajogaite Eruption: The ISVOLCAN Study in Spain. [PDF]
Simbaña-Rivera K +9 more
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Precise dating of large flank collapses by single-grain 40Ar/39Ar on pyroclastic deposits from the example of Flores Island (Azores). [PDF]
Hildenbrand A +4 more
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Volcanic eruptions and the global subsea telecommunications network. [PDF]
Clare MA +22 more
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Direct observation of degassing during decompression of basaltic magma. [PDF]
Bonechi B +11 more
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Hydrothermal calcite formation in Campi Flegrei caldera, Italy: unraveling carbon sink processes in alkaline volcanic systems. [PDF]
Buono G +3 more
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First Report of <i>Acanthamoeba</i> Genotype T4 from the Newly Formed Tajogaite Volcano Tephra (La Palma, Canary Islands). [PDF]
Pérez-Pérez P +9 more
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The spatiotemporal evolution of compound impacts from lava flow and tephra fallout on buildings: lessons from the 2021 Tajogaite eruption (La Palma, Spain). [PDF]
Biass S +7 more
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Scoria cone formation through a violenmt Strombolian eruption : Ira Volcano, SW Japan
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Laboratory models of Hawaiian and Strombolian eruptions
Nature, 1988Basaltic eruptions are often characterized by cyclic changes of activity. At Hawaii, periods of continuous fountaining alternate with much longer periods of effusive outflow1,2. In Strombolian eruptions, activity proceeds through intermittent discrete bursts2–5. We report laboratory experiments that simulate the degassing process in basaltic eruptions.
Claude Jaupart, Sylvie Vergniolle
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