Growth of the lava dome and extrusion rates at Soufrière Hills Volcano, Montserrat, West Indies: 2005-2008

Author:

Ryan G. A.,Loughlin S. C.,James M. R.1,Jones L. D.,Calder E. S.2,Christopher T.,Strutt M. H.,Wadge G.3

Affiliation:

1. Lancaster Environment Centre; Lancaster University; Lancaster; UK

2. Department of Geology; State University of New York at Buffalo; Buffalo; New York; USA

3. Environmental Systems Science Centre; University of Reading; Reading; UK

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference24 articles.

1. Geol. Soc. London Mem.;Bonadonna,2002

2. Mobility of pyroclastic flows and surges at the Soufrière Hills Volcano, Montserrat;Calder;Geophys. Res. Lett.,1999

3. Geol. Soc. London Mem.;Calder,2002

4. Control of magma flow in dykes on cyclic lava dome extrusion;Costa;Geophys. Res. Lett.,2007

5. Petrologic determination of ascent rates for the 1995-1997 Soufrière Hills Volcano andesitic magma;Devine;Geophys. Res. Lett.,1998

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