Lava Flows and Domes: Emplacement Mechanisms and Hazard Implications

Portada
Jonathan H. Fink
Springer Science & Business Media, 6 de des. 2012 - 249 pàgines
This collection of papers is based on a symposium held in 1987 at the Interna tional Union of Geology and Geodesy Congress in Vancouver, British Colum bia. The Symposium was planned as a follow-up to a session at the 1984 Geo logical Society of America Annual Meeting in Reno, Nevada, which dealt with the emplacement of silicic lava domes. In both cases, emphasis was placed on the physical and mechanical rather than chemical aspects of lava flow. The IUGG Symposium consisted of two lecture sessions, a poster session, and two discussion periods, and had 22 participants. The contributions to this volume are all based on papers presented in the various parts of the Sym posium. The motivation for studying lava flow mechanics is both practical and scientific. Scientists and government agencies seek to more effectively predict the hazards associated with active lavas. Recovering mineral resources found in lava flows and domes also requires an understanding of their emplacement. From a more theoretical standpoint, petrologists view lava studies as a way to directly observe the rheologic consequences of mixing crystals, bubbles, and solid blocks of country rock with silicate liquids. This information can then be used to constrain processes occurring in the concealed conduits, dikes, and chambers that feed flows and domes on the surface.
 

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Table of Contents
4Change inHeight
References
5Discussion
3Observations 4Resultsand Discussion
5Conclusions and Unresolved Questions
3Theoretical Models of the Flow of Low LavaDomes
Application to a Dome Building Eruption at Mount St Helens
Method
Morphology Rheology Crystallization and Scaling Phenomena
4Cauliflower
Concluding Comments
4Discussion
Program for Simulation
Copyright

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