Titlebook: Volcanic Debris Avalanches; From Collapse to Haz Matteo Roverato,Anja Dufresne,Jonathan Procter Book 2021 Springer Nature Switzerland AG 20

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Volcanic Debris Avalanches: Introduction and Book Structure,g of their history and global distribution, collapse initiation and cyclic occurrence, problems with terminology, transport processes and deposit characteristics, climate impacts, application of numerical tools, and the records of marine and ringplain settings.

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Volcanic Debris Avalanches: Introduction and Book Structure,cture. This first chapter aims to introduce a collection of themed papers gathered in a book, each illustrating the advancements of a different aspect of VDA research. As a state-of-the-art collection, the 11 papers provide a powerful tool for the volcanological community to enhance our understandin

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Terminology and Strategy to Describe Large Volcanic Landslides and Debris Avalanches,ortion(s) of a volcanic edifice. In this chapter, we evaluated the current terminology used to describe this phenomenon. We propose a descriptive scheme based on metrics and geological features that allows us to extract significant information from both the source area and the deposit. The landslide

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Factors Contributing to Volcano Lateral Collapse,over hundreds to more than a thousand km. with debris. Volcanic lateral collapses are severe hazards because of their destructive power and size, and sudden onset. Although their frequency of occurrence is not as high as those of smaller volcanic mass movements, such as rock falls and lahars, global

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Climatic Influence on Volcanic Landslides,imate. In this chapter, we consider the influences of present and geologically recent climates on the occurrence of volcanic landslides. We begin by summarizing Quaternary climatic variability to illustrate the wide range of conditions and rates of change experienced by modern edifices. A focus on g

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Volcanic Debris Avalanche Transport and Emplacement Mechanisms,amic behaviour. These include ., ., and sliding along ., none of which involve large-scale turbulence during transport. The plug flow model shows normal gradation in the plug, and reverse grading in the laminar boundary layers. During translational sliding, spreading of the mass is accommodated by l

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Sedimentology of Volcanic Debris Avalanche Deposits,e summarize the sedimentary characteristics and the different (litho-)facies described over the past four decades, and how findings from individual case studies can be adapted as globally applicable sedimentological tools. A plethora of descriptive terms and partially conflicting definitions emerged

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