Titlebook: Volcanology; Processes, Deposits, Ray Cas,Guido Giordano,John V. Wright Textbook 2024Latest edition Springer Nature Switzerland AG 2024 Vol

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High-Viscosity Silicic Lavas (Rhyolite, Dacite, and Andesite)ountry rock assimilation, usually in crustal magma reservoirs, generate felsic magma bodies with progressively lower temperature, increasing silica content and higher viscosity. These in turn affect the mobility, flow distance of any erupted lava flow which generally decreases as the SiO. content an

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annexation

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Explosive Eruption Styles, Columns, and Pyroclastic Fallout Deposits produce pyroclastic fallout deposits. At the small-scale end of the spectrum of subaerial explosive eruptions, we include strombolian ., halema’ma’uan and small-scale vulcanian and hydrothermal explosions. At the next level, there are small-scale hawai’ian magma/fire fountaining and larger scale vu

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Subaqueous Flows of Pyroclastic Debris and Their Depositssubaerial vents, or are erupted from subaqueous vents. Does dynamic interaction with the ambient water mass occur? Do the flows mix in ambient water, and transform from hot, gas-supported pyroclastic (mass) flows into water-supported mass flows (e.g. syn-eruptive debris flows and megaturbidity curre

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Surface Sedimentary (Epiclastic) Processes and Deposits in Volcanic Environments8) have been marked by major-impact sedimentary events both during and immediately after their respective eruptions. These secondary events have produced at least as much damage to infrastructure as the primary eruption processes, and have led to numerous deaths. In the case of the Mt Pinatubo erupt

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Syn- to Post-emplacement Alteration Processessuccessions. These processes include devitrification, palagonitisation (in mafic glass), hydrothermal alteration, diagenesis, metamorphism, and tectonic deformation, which may significantly modify and in some cases completely disguise original volcanic textures. The process that induces textural cha

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Textbook 2024Latest editionded into six major parts, it offers comprehensive information on magma properties; fragmentation processes; subaerial and subaqueous lava types and field textures; sub-volcanic intrusions; explosive or pyroclastic eruptions and deposits; surface sedimentary processes; hydrothermal alteration and lit