Glossary
- Conduit :
-
Subterranean pathways to the surface created and sustained by the flow of volcanic materials are known as volcanic conduits. In the laboratory, tubes are used as scale equivalents. The two terminologies (‘conduits’ and ‘tubes’) should be kept distinct to avoid inadvertent acceptance that a laboratory experiment is a direct replica of a volcanic process.
- Magma :
-
When rock melts underground it becomes magma. When magma flows on the surface it is known as lava and when it is projected into the atmosphere it forms pyroclasts. Most magma is silicate-based and comprises a three-phase mixture of solid (crystals, called microlites when small), liquid (melt) and gas (bubbles or vesicles).
- Rheology :
-
When a force is applied to matter it deforms. The rheology of a material describes the relationship between applied force and the material response. Volcanic materials have a wide range of rheological behaviors dependent on the proportions of gas, liquid and solid, temperature,...
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Acknowledgments
We thank Bernard Chouet for a highly constructive review of this chapter, William H. K. Lee for editing this section and the staff at Springer including Julia Koerting and Kerstin Kindler.
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Lane, S.J., James, M.R. (2009). Volcanic Eruptions, Explosive: Experimental Insights. In: Tilling, R.I. (eds) Complexity in Tsunamis, Volcanoes, and their Hazards. Encyclopedia of Complexity and Systems Science Series. Springer, New York, NY. https://doi.org/10.1007/978-1-0716-1705-2_579
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