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

The Canadian Cordillera hosts numerous Pleistocene and Holocene volcanoes and
volcanic deposits, including a number of volcanoes that have erupted within the last several …

Abstract The West Antarctic Ice Sheet overlies the West Antarctic Rift System about which,
due to the comprehensive ice cover, we have only limited and sporadic knowledge of …

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 …

The 13-day-long Gjálp eruption within the Vatnajökull ice cap in October 1996 provided
important data on ice–volcano interaction in a thick temperate glacier. The eruption …

Basaltic pahoehoe lava-fed deltas are important coastal constructions of many oceanic
islands and continental flood basalt provinces. Whilst littoral processes associated with their …

Ruapehu is an active~ 150 km 3 andesite-dacite composite volcano located at the southern
end of the Taupo Volcanic Zone, New Zealand. The growth of the present-day edifice has …

Ice exerts a first-order control over the distribution and preservation of eruptive products on
glaciated volcanoes. Defining the temporal and spatial distributions of ice-marginal lava …

Kitasu Hill and MacGregor Cone formed along the Principe Laredo Fault on British
Columbia's central coast as the Wisconsinan ice sheet withdrew from the Coast Mountains …

Eruptions within glaciers are characterized by fast cooling of volcanic deposits, rapid melting
of ice and heating of meltwater. Heat transfer rates in subglacial eruptions may be monitored …