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Non-linear flow modelling of a Martian Lobate Debris Apron
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Atmospheric processes affecting the separation of volcanic ash and SO2 in volcan...
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Assessing Impact to Infrastructures Due to Tephra Fallout From Öræfajökull Volca...
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Millennial-scale fluctuations in Saharan dust supply across the decline of the A...
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Western Mediterranean hydro-climatic consequences of Holocene ice-rafted debris...
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Volatile and light lithophile elements in high-anorthite plagioclase-hosted melt...
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Satellite detection, long-range transport, and air quality impacts of volcanic s...
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Rootless tephra stratigraphy and emplacement processes
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Climate variability in the past ∼19,000 yr in NE Tibetan Plateau inferred from b...
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Tracking Holocene drift-ice limits on the northwest–southwest Iceland shelf: Com...
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Postglacial relative sea level change and glacier activity in the early and late...
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Postglacial relative sea-level changes in northwest Iceland: Evidence from isola...
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The onset of neoglaciation in Iceland and the 4.2 ka event
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Magmatic crystal records in time, space, and process, causatively linked with vo...
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Impact of Icelandic dust and volcanic ash on snow and ice
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Subglacial hydrology of the Icelandic ice caps: Outburst floods and ice dynamics
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Ground deformation caused by viscoelastic relaxation and its role in the 2015-20...
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Short- and Long-term Model Simulations of the Evolution of Vatnajökull Ice Cap
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Explosive activity in flood lava eruptions: a case study of the 10th century Eld...
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Breiðdalur Central Volcano. What came first: the central volcano or the fissure...
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