Shape evolution of pumice during granular flow. [PDF]
Figueiredo C +5 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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A Tale of Two Shrimps-Speciation and Demography of Two Sympatric Shrimp Species From Hydrothermal Vents. [PDF]
Methou P +5 more
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Identification of tephras erupted from Iwate Volcano after the Toya Ash falling.
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Protist ecology in Patagonian peatlands: pH, organic phosphorus, and sulfate as key drivers of testate amoeba diversity in undisturbed ecosystems. [PDF]
Fernández LD +3 more
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Understanding paleo-earthquakes in the Kuril Trench based on Late-Holocene tsunami deposits in the distal region from wave sources, northern Hidaka, Hokkaido, Japan. [PDF]
Nakanishi R +4 more
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The Minoan Thera eruption predates Pharaoh Ahmose: Radiocarbon dating of Egyptian 17th to early 18th Dynasty museum objects. [PDF]
Bruins HJ, van der Plicht J.
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Sustainable Use of Volcanic Ash in Mortars as a Replacement for Cement or Sand: Shrinkage and Physical and Mechanical Properties. [PDF]
Gil-Martín LM +4 more
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Plinian and co-ignimbrite tephra fall from the
Bulletin of Volcanology, 1989A study of pyroclastic deposits from the 1815 Tambora eruption reveals two distinct phases of activity, i.e., four initial tephra falls followed by generation of pyroclastic flows and the production of major co-ignimbrite ash fall. The first explosive event produced minor ash fall from phreatomagmatic explosions (F-1 layer).
Sigurdsson, Haraldur, Carey, Steven
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Total grain-size distribution and volume of tephra-fall deposits
Bulletin of Volcanology, 2005On 17 June 1996, Ruapehu volcano, New Zealand, produced a sustained andesitic sub-Plinian eruption, which generated a narrow tephra-fall deposit extending more than 200 km from the volcano. The extremely detailed data set from this eruption allowed methods for the determination of total grain-size distribution and volume of tephra-fall deposits to be ...
Bonadonna, Costanza, Houghton, B.F.
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