In: Bulletin of Volcanology, 2015, vol. 77, no. 2, p. 1-19
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In: Bulletin of Volcanology, 2015, vol. 77, no. 7, p. 1-12
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In: Contributions to Mineralogy and Petrology, 2015, vol. 170, no. 5-6, p. 1-18
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In: International Journal of Earth Sciences, 2015, vol. 104, no. 7, p. 1795-1817
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In: Journal of Paleolimnology, 2015, vol. 54, no. 1, p. 137-152
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In: Bulletin of Volcanology, 2015, vol. 77, no. 11, p. 1-14
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In: Environmental Research, 2019, vol. 179, p. 108798
Volcanic plumes are complex environments composed of gases and ash particles, where chemical and physical processes occur at different temperature and compositional regimes. Commonly, soluble sulphate- and chloride-bearing salts are formed on ash as gases interact with ash surfaces. Exposure to respirable volcanic ash following an eruption is potentially a significant health concern. The...
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In: Nature Geoscience, 2019, vol. 12, no. 8, p. 650–656
During the first half of the nineteenth century, several large tropical volcanic eruptions occurred within less than three decades. The global climate effects of the 1815 Tambora eruption have been investigated, but those of an eruption in 1808 or 1809 whose source is unknown and the eruptions in the 1820s and 1830s have received less attention. Here we analyse the effect of the sequence of...
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In: European Journal of Wildlife Research, 2014, vol. 60, no. 4, p. 699-702
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In: Journal of Volcanology and Geothermal Research, 2018, vol. 359, p. 47–67
The subduction-related volcanic front in Nicaragua consists of the Tertiary “Coyol” member in the eastern highlands and the Quaternary to recent volcanic arc within the Nicaraguan depression. Although the Holocene to recent explosive volcanism has been studied extensively no detailed work has been done on the products of explosive volcanism from Quaternary volcanic complexes comprising...
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