This paper describes unusual rhyolitic deposits at Dalakvísl, Torfajökull, Iceland that were emplaced during a Quaternary subglacial eruption. Despite its small volume (<0.2 km3), the eruption mechanisms were highly variable and involved both explosive and intrusive phases. The explosive phase involved vesiculation-driven magma fragmentation at the glacier base and generated a pumiceous pyroclastic deposit containing deformed sheets of dense obsidian. Textures suggest that the obsidian was generated by the collapse of partly fragmented foam that was intruding the deposit and water contents indicate quenching at elevated pressures. In contrast, the intrusive phase of the eruption generated vesicle-poor quench hyaloclastites associated with a...
Eruptions of Öræfajökull have produced mafic and silicic magmas, and have taken place in both glacia...
An eruption along a 2.5 km-long rhyolitic dyke at Krafla volcano, northern Iceland during the last g...
Simple analytical models of subglacial eruptions are presented, which simulate evolving subglacial c...
This paper describes unusual rhyolitic deposits at Dalakvisl, Torfajokull, Iceland that were emplace...
Abstract. We present field observations from Blahnukur, a small volume (400 m thick. Lithofacies ass...
Simple analytical models of subglacial eruptions are presented, which simulate evolving subglacial c...
We present the first modern volcanological study of a subglacial-to-emergent rhyolite tuya, at SE Ra...
Rhyolite eruptions in Iceland mostly take place at long-lived central volcanoes, examples of which a...
Rhyolitic eruptions beneath Icelandic glaciers can be highly explosive, as demonstrated by Quaternar...
Rhyolite eruptions in Iceland mostly take place at long-lived central volcanoes, examples of which a...
Subglacial rhyolite eruptions at Torfajökull, Iceland have produced a variety of volcanic edifices d...
Eruptions of Öræfajökull have produced mafic and silicic magmas, and have taken place in both glacia...
Although observations of recent volcanic eruptions beneath Vatnajokull, Iceland have improved the un...
Many volcanoes express a variety of contrasting eruptive styles with behavioural transitions between...
Large scale subglacial eruptions are enigmatic. Their eruption and emplacement dynamics are not wel...
Eruptions of Öræfajökull have produced mafic and silicic magmas, and have taken place in both glacia...
An eruption along a 2.5 km-long rhyolitic dyke at Krafla volcano, northern Iceland during the last g...
Simple analytical models of subglacial eruptions are presented, which simulate evolving subglacial c...
This paper describes unusual rhyolitic deposits at Dalakvisl, Torfajokull, Iceland that were emplace...
Abstract. We present field observations from Blahnukur, a small volume (400 m thick. Lithofacies ass...
Simple analytical models of subglacial eruptions are presented, which simulate evolving subglacial c...
We present the first modern volcanological study of a subglacial-to-emergent rhyolite tuya, at SE Ra...
Rhyolite eruptions in Iceland mostly take place at long-lived central volcanoes, examples of which a...
Rhyolitic eruptions beneath Icelandic glaciers can be highly explosive, as demonstrated by Quaternar...
Rhyolite eruptions in Iceland mostly take place at long-lived central volcanoes, examples of which a...
Subglacial rhyolite eruptions at Torfajökull, Iceland have produced a variety of volcanic edifices d...
Eruptions of Öræfajökull have produced mafic and silicic magmas, and have taken place in both glacia...
Although observations of recent volcanic eruptions beneath Vatnajokull, Iceland have improved the un...
Many volcanoes express a variety of contrasting eruptive styles with behavioural transitions between...
Large scale subglacial eruptions are enigmatic. Their eruption and emplacement dynamics are not wel...
Eruptions of Öræfajökull have produced mafic and silicic magmas, and have taken place in both glacia...
An eruption along a 2.5 km-long rhyolitic dyke at Krafla volcano, northern Iceland during the last g...
Simple analytical models of subglacial eruptions are presented, which simulate evolving subglacial c...