Martin, Michael Dieter , Barr, Iestyn , Edwards, Benjamin R. , Spagnolo, Matteo , Vajedian, Sanaz , and Symeonakis, Elias

Globally, about 250 Holocene volcanoes are either glacier-clad or have glaciers in close proximity. Interactions between volcanoes and glaciers are therefore common, and some of the most deadly (e.g., Nevado del Ruiz, 1985) and...

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Pollock, Meagen , Edwards, Benjamin R. , Judge, Shelley, Wallace, Chloe, Hiatt, Alex, Perpalaj, Aleksander, Was, Ellie, and Hauksdóttir, Steinunn

Glaciovolcanic landforms provide global-scale records of paleoenvironmental conditions and yield insights into subglacial eruption processes. Models for the formation of glaciovolcanic ridges, or tindars, are relatively simple,...

Article

Edwards, Benjamin R. , Russell, James K. , and Pollock, Meagen

In contrast to water and air, ice is the most dynamic enveloping medium and unique environment for volcanic eruptions. While all three environments influence volcanic activity and eruption products, the cryospheric eruption...

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Russell, James K., Edwards, Benjamin R. , Williams-Jones, Glyn, and Hickson, Catherine J.

The Canadian Cordillera hosts numerous Pleistocene and Holocene volcanoes and volcanic deposits, including a number of volcanoes that have erupted within the last several hundred years. The nature and composition of volcanic...

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Edwards, Benjamin R. , Belousov, A. , and Belousova, M.

Understanding interactions between volcanic eruptions and the cryosphere (a.k.a. glaciovolcanism) is important for climate reconstructions as well as for hazard mitigation at ice-clad volcanoes. Here we present unique field...

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