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- W2061253198 abstract "Pyroclastic flow is defined as the flow of high-temperature, essential, fragmental materials. This is synonymous with the nuee ardente in the broad sense. Three modes of emplacement of high-temperature, essential, solid (or liquid) materials after the ejection from the crater may be recognized: 1) Projection of fragments from the crater by explosive expansion of gas within the crater; 2) descent of fragments or liquid magma from the crater caused only by the action of gravity; and 3) swift downflow of the mixture of gas and fragments. This last is intermediate between the first two and corresponds to pyroclastic flow. A new classification of pyroclastic flows is proposed based upon viscosity of the materials, which ls inferred from the nature of the deposit. The volume of the deposit increases as the viscosity decreases. 1) Nuee ardente in the strict sense: Represented by the nuee ardente of Mt. Pelee, Merapi, etc. The fragments are less porous, which indicates the high viscosity. The volume of the deposi..." @default.
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- W2061253198 date "1961-06-01" @default.
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- W2061253198 title "CLASSIFICATION OF PYROCLASTIC FLOWS" @default.
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