We present a descriptive genetic classification scheme and accompanying nomenclature for
glaciovolcanic edifices herein defined as tuyas: positive-relief volcanoes having a …

In this paper, we examine the nature of the Pliocene Antarctic Peninsula Ice Sheet by
comparing the terrestrial and marine geological records of the Antarctic Peninsula and …

The study of volcano-ice interactions, or'glaciovolcanism', is a field experiencing exponential
growth. This comprehensive volume presents a discussion of the distinctive processes and …

An eruption along a 2.5 km-long rhyolitic dyke at Krafla volcano, northern Iceland during the
last glacial period formed a ridge of obsidian (Hrafntinnuhryggur). The ridge rises up to 80 m …

Analysis of the spatial lithofacies variability within lava-fed delta formations in southern
Iceland has revealed complex three-dimensional volcanic architectures in hyaloclastite …

Abstract The Late-Miocene Torfufell central volcano (ToCV), situated between the now
extinct Snæfellsnes-Húnaflói rift zone and the presently active rift in North Iceland, provides …

Volcanoes that interact with the cryosphere preserve indicators of their eruption
environments. These glaciovolcanoes and their deposits have powerful potential as proxies …

The degassing of magmatic volatiles during eruptions beneath ice sheets and glaciers, as
recorded by the dissolved volatile content quenched in volcanic rocks, could provide …

Subglacially-erupted volcanic sequences provide proxies for a unique range of palaeo-ice
parameters and they are potentially highly useful archives of palaeoenvironmental …

Passage zones are stratigraphic surfaces found in littoral settings separating deposits
diagnostic of subaqueous environments from overlying sequences of subaerial deposits. In …