A thermodynamical model for rainfall‐triggered volcanic dome collapse
- 12 March 2004
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 31 (5)
- https://doi.org/10.1029/2003gl019310
Abstract
No abstract availableKeywords
This publication has 11 references indexed in Scilit:
- Instability of exogenous lava lobes during intense rainfallBulletin of Volcanology, 2004
- Anatomy of a lava dome collapse: the 20 March 2000 event at Soufrière Hills Volcano, MontserratJournal of Volcanology and Geothermal Research, 2004
- Rainfall‐induced volcanic activity on MontserratGeophysical Research Letters, 2002
- Mineral disequilibrium in lavas explained by convective self-mixing in open magma chambersNature, 2001
- Control on the emplacement of the andesite lava dome of the Soufriere Hills volcano, Montserrat by degassing‐induced crystallizationTerra Nova, 2000
- Nonlinear dynamics of lava dome extrusionNature, 1999
- Experimental phase equilibria constraints on pre‐eruptive storage conditions of the Soufriere Hills magmaGeophysical Research Letters, 1998
- The initial cooling of pahoehoe flow lobesBulletin of Volcanology, 1996
- Infrared image analysis of volcanic thermal features: Láscar Volcano, Chile, 1984–1992Journal of Geophysical Research, 1993
- Cooling rate and thermal structure determined from progressive magnetization of the Dacite Dome at Mount St. Helens, WashingtonJournal of Geophysical Research, 1990