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 …

Glaciovolcanism produces distinctive features that are useful paleoclimate proxies for the
distribution of past ice sheets and glacier extent. The Copahue volcano located in the …

Magma–ice–meltwater interactions produce diverse landforms and lithofacies, reflecting the
multitude of factors that influence glaciovolcanism, including both magmatic (eg …

Understanding lava flow processes is important for interpreting existing lavas and for hazard
assessments. Although substantial progress has been made for basaltic lavas our …

Glacial outburst floods (jökulhlaups1) are a potent hazard in the proximal and distal regions
of an erupting subglacial volcano (Tilling, 1989; Roberts, 2005; Gudmundsson et al., 2008) …

Located in a poorly studied zone of the rear arc in the Transitional Southern Volcanic Zone,
the Overo volcano presents a complete record of syn-glacial, inter-glacial, and post-glacial …

Permeability hosted in andesitic lava flows is dominantly controlled by fracture systems, with
geometries that are often poorly constrained. This paper explores the fracture system …

ABSTRACT The Tuya-Kawdy region of northern British Columbia is well established as a
place where glaciation and volcanism overlapped in space. However, no modern work has …

Several broadly circular structures up to 16 m in diameter, into which higher strata have
sagged and locally collapsed, are present in a tephra outcrop on southwest Öræfajökull …

Globally there is an abundance of geothermal resources that are suitable for low enthalpy
geothermal energy generation, such as ground source heating however, very few of these …