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Home > Research > Researchers > Hugh Tuffen
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Hugh Tuffen supervises 3 postgraduate research students. Some of the students have produced research profiles, these are listed below:

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Dr Hugh Tuffen

Research Fellow/Lecturer

Hugh Tuffen

LEC Building

Lancaster University

Bailrigg

Lancaster LA1 4YQ

United Kingdom

Tel: +44 1524 594713

Location:

Research overview

Hugh is a volcanologist, Royal Society University Research Fellow and Lecturer in LEC. He is fascinated by the power and beauty of volcanoes, and committed to help better understand their behaviour to assist the many millions threatened by volcanic activity. His uses a combination of fieldwork, geochemical analysis, experimentation and modelling to investigate key eruption-controlling processes.

Research Interests

Current research interests include:

How does gas escape from highly-viscous, silica-rich magma?

Tuffisite veins are formed by venting of gas and ash through fractures in and around conduits and lava domes, as seen in my 2012 BBC2 film from Cordon Caulle. They are thought to be key eruption controls, mediating the escape of gas from highly-viscous magma, and responisble for earthquake triggering in silicic eruptions. However, they are also known to seal up, preventing pressure release and driving explosions. Little is understood about the timescale and mechanism of tuffisite formation, the amount of gas they can deliver, and how rapidly they become blocked and sealed. We are using field and micro-textural methods to characterise the nature of tuffisite veins from a depth of hundreds of metres in conduits up to the surface. Measurement of volatile species is proving particularly useful as a tool to reconstruct pressure changes during vein venting and blockage. This work is supported by the Royal Society and NERC and carried out in collaboration with scientists at the University of Mainz and McGill University.

 

What controls the explosivity of sub-ice eruptions?

A large proportion of the world's volcanoes are at least partly ice-covered, most notably in Iceland, and this makes them more hazardous, as magma interacts explosively with meltwater  and rapid ice melting generates powerful floods. We know remarkably little about this type of eruption, for example whether Icelandic ash plumes such as Eyjafjalljokull 2010 are driven by dissolved volcanic gases or interactions with meltwater. AXA postdoctoral research fellow Jacqueline Owen is investigating what controlled the powerful 1918 eruption of Katla volcano in Iceland, having completed an in-depth study of the largest known sub-ice rhyolitic eruption, from nearby Torfajokull.

 

What controls lava flow advance?

Lava has a broad range of compositions, from low-silica basalt to high-silica rhyolite. Dramatic differences in viscosity (by several orders of magnitude) mean that basaltic lavas can advance hundreds of times more rapidly that rhyolites. However, there appear to be common processes controlling lava advance and the evolution of flow fields. We recently made the first detailed observations of an active rhyolitic lava flow, at Cordon Caulle in Chile, and discovered that slowly-moving rhyolite (1-3 metres a day) behaves in a very similar way to more fluid and commonplace basalts. In ongoing research, supported by the Royal Society and NERC, we are characterising and contrasting rhyolite lava advance at Cordon Caulle with basaltic flows at Bardarbunga, Iceland and Etna, Italy.

 

How does magma crystallise, degas and vesiculate?

The growth of crystals and bubbles in magma, and the loss of dissolved gases, has a transformative effect on its behaviour. For example, crystallisation mediates crust formation in lava flows, vesiculation controls the formation of magmatic foams during explosive events, and degassing determines whether explosive or effusive eruptions occur. We are using two complimentary approaches: experimentally growing crystals and vesicles in magmas in the lab to measure rates and patterns of growth, and characterising crystal and vesicle populations in ancient rocks to reconstruct what happened. Similarly, experimental degassing compliments measurement of dissolved gases in natural volcanic glasses. This research is supported by the Royal Society and AXA.

Research Grants

2013       AXA Postdoctoral Fellowship, PI, £110k, Understanding Katla, Iceland’s notorious and restless volcano: Lessons from 1918.

2012       Royal Society Equipment Grant, PI, £50k, Differential Scanning Calorimetry.

2011       NERC small grant NE/I016414/1 co-I, £65k, “Quantifying degassing-driven crystal growth in basaltic lavas”.

2010       Royal Society University Research Fellowship, PI, £563 k, 2010-2015.

2009       NERC standard grant NE/F018010/1, Co-I, £370 k, “The effects of degassing and effusion rate fluctuations on the evolution of basaltic flow fields”.

2008       NERC New Investigator grant NE/G000654/1, “Volatile degassing from magma: Insights from eruptions under Icelandic glaciers”, PI, 2008-2010, £6k.

2007       NERC Research Fellowship NE/E013740/1, PI, £260k.

2006       NERC standard grant NE/D012910/1, researcher co-I, £550 k (£21k to Lancaster), “Fracture mechanics of dome lava”.

2004       Leverhulme Early Career Research Fellowship, Lancaster-UCL, PI, £90 k.

Current Teaching

LEC478 Physical Volcanology

My Role

Royal Society University Research Fellow and Lecturer

Director of Studies, MSc in Volcanology and Geological Hazards

Other Interests and Hobbies

By night Hugh plays 'cello with The Balkanics.

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