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• W2236655024 abstract "Most of Etna’s historical lavas have produced aa flow-fields. Despite the classification, they support a variety of surfaces in both the pahoehoe and aa categories. From observations of surface features at metre to submillimetre scales, two morphological series have been recognized: a sequence from pahoehoe to aa along a single flow, and an evolutionary trend among pahoehoe surfaces near boccas down a flow-field. The first series is more prominent and is superimposed on the second. Both series are associated with increasing crystallinity. The pahoehoe-aa sequence, however, is characterized by relatively higher crystallization rates and shear rates, indicating greater undercoolings and imposed stresses during emplacement. The identification of crystallization rate as a controlling factor demonstrates the influence of crystallization kinetics on lava development. The pahoehoe-aa transition also shows evidence of self-similar patterns at scales from at least millimetres to tens of centimetres, and may be accompanied by a self-feeding mechanism which couples large- and small-scale changes in lava rheology and shear rate." @default.
• W2236655024 created "2016-06-24" @default.
• W2236655024 creator A5042459263 @default.
• W2236655024 date "1990-01-01" @default.
• W2236655024 modified "2023-09-26" @default.
• W2236655024 title "Surfaces of Aa Flow-Fields on Mount Etna, Sicily: Morphology, Rheology, Crystallization and Scaling Phenomena" @default.
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• W2236655024 doi "https://doi.org/10.1007/978-3-642-74379-5_6" @default.
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