Hydrovolcanism is a type of volcanism where magma and water interact either explosively or
non-explosively. The less frequently used term, hydromagmatism, includes all the processes …

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

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 …

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 …

Volcanic rocks are important in compiling geological records because of their characteristic
chemistry, relatively fast accumulation and great variety; however, recognizable facies …

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 …

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

Iceland contains an abundance and diversity of rhyolitic edifices produced during volcano–
ice interactions (glaciovolcanism) that is unmatched by any other volcanic province, with an …

Variable eruptive style and explosivity is common in basaltic to basaltic andesite volcanoes
but can have uncertain origins. Veniaminof volcano in the Alaska-Aleutian arc is a frequently …