V23F:
How and When Do Volcanic Eruptions Start and Stop, and What Controls the Tempo of Everything in Between? I


Session ID#: 8269

Session Description:
There is much information now accumulating about the timing of volcanic eruptions, from the millennia (or longer) for the accumulation of magma into its eruptible state through to real-time observations of contemporary eruptive activity. A key aim of volcanology is to forecast the course of future events and provide advice on the timing and processes at ongoing eruptions on timescales that are relevant to humanity and with a degree of confidence about the processes involved. We invite contributions that address all the facets of this topic. These might include (1) magmatic forensics of past eruption products that contribute to accurate assessment of timescales and processes in past events; (2) studies of modern eruptions and the controls on their durations, including prolonged, multi-episode events; and (3) how temporal information about magmatic and volcanic processes can be translated into sound and useful advice to civil authorities for managing ongoing and future events.
Primary Convener:  Colin J N Wilson, Victoria University of Wellington, Wellington, New Zealand
Conveners:  Michelle L Coombs, Alaska Volcano Observatory Anchorage, USGS, Anchorage, AK, United States, Bruce F Houghton, University of Otago, Dunedin, New Zealand and Paul J Wallace, University of Oregon, Department of Earth Sciences, Eugene, United States
Chairs:  Colin J N Wilson, Victoria University of Wellington, Wellington, New Zealand and Michelle L Coombs, Alaska Volcano Observatory Fairbanks, Fairbanks, United States
OSPA Liaison:  Colin J N Wilson, Victoria University of Wellington, Wellington, New Zealand

Abstracts Submitted to this Session:

Allison E Rubin1,2, Kari M Cooper2, Adam JR Kent3, Fidel Costa Rodriguez4 and Christy B. Till5, (1)University of California Davis, Davis, CA, United States, (2)University of California Davis, Earth and Planetary Sciences, Davis, CA, United States, (3)Oregon State University, College of Earth, Ocean, & Atmospheric Sciences, Corvallis, OR, United States, (4)Nanyang Technological University, Singapore, Singapore, (5)Arizona State University, School of Earth & Space Exploration, Tempe, AZ, United States
R Stephen J Sparks and Katharine V Cashman, University of Bristol, Bristol, United Kingdom
Samantha Tramontano1, Guilherme A R Gualda1, Mark S Ghiorso2 and Ben Kennedy3, (1)Vanderbilt University, Earth and Environmental Sciences, Nashville, TN, United States, (2)OFM Research, Redmond, CA, United States, (3)University of Canterbury, School of Earth and Environment, Christchurch, New Zealand
Sarah E Ogburn1, Robert Wolpert2, Eliza Calder3, John S Pallister1 and Heather Michelle Nicholson Wright1, (1)USGS Cascades Volcano Observatory, Vancouver, WA, United States, (2)Duke University, Department of Statistical Science, Durham, NC, United States, (3)University of Edinburgh, School of GeoSciences, Edinburgh, United Kingdom
Kevin A Reath, University of Pittsburgh Pittsburgh Campus, Department of Geology and Planetary Science, Pittsburgh, PA, United States, Matthew Watson, University of Bristol, Earth Sciences, Bristol, United Kingdom and Michael S Ramsey, University of Pittsburgh, Department of Geology and Environmental Science, Pittsburgh, PA, United States
Marie Edmonds, University of Cambridge, Department of Earth Sciences, Cambridge, United Kingdom and Brendan T McCormick, University of Cambridge, Cambridge, United Kingdom