The thermal evolution and dynamics of pyroclasts and pyroclastic density currents
The thermal evolution of pyroclastic density currents (PDCs) is the result of entrainment of ambient air, particle concentration, and initial eruptive temperature, which all impact PDC dynamics and their hazards, such as runout distance. The associated hazards and opaqueness of PDCs make it impossib...
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Format: | Others |
Language: | en_US |
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Georgia Institute of Technology
2015
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Online Access: | http://hdl.handle.net/1853/53962 |