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-Island Lateral Collapses and Their Submarine Deposits,heir continental equivalents, and can generate devastating tsunamis. All historical volcanic-island lateral collapses have occurred in arc settings, and have been characterised by rapid failure and efficient tsunami generation. The varied morphology of their deposits is influenced both by lithologic

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Computer Simulation of a Volcanic Debris Avalanche from Mt. Taranaki, New Zealand,igh-magnitude but low-frequency hazard facing the surrounding community. The ~7000?yr B.P. Opua Formation is the youngest of these events and exhibits the typical chaotic, polymodal, polylithologic and extremely poorly sorted characteristics of DADs. Despite the apparent invariance of these large-sc

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Book 2021 phenomenon. It has been 40 years since the volcanic debris avalanche associated with the 1980 eruption of Mount St. Helens, and our understanding of these events has grown considerably in the interim. Drawing on these advances, the book addresses all aspects of volcanic debris avalanches. Though pr

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A Historical Perspective on Lateral Collapse and Volcanic Debris Avalanches,ts after 1980 has led to an average of one regional or global debris-avalanche inventory annually in terrestrial or submarine settings and the recognition of a thousand events from nearly 600 volcanoes. The last major volcaniclastic process to be widely recognized and understood, large-volume debris

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Distribution and Geometric Parameters of Volcanic Debris Avalanche Deposits,is is mainly due to differences in source scar geometry. At the same drop height, VDAs can produce larger volumes because their scars are deeper-seated, more bowl-shaped, and extend along longer slopes than is common for rock slopes. Although the new database is still incomplete, this compilation sh

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Climatic Influence on Volcanic Landslides,g triggers of volcanic landslides. Finally, case studies of present and past climate influences on volcanic landslides collected from scientific literature–covering both subaerial and coastal settings–illustrate several key points: edifice collapses were numerous at the end of the last glaciation; c

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Volcanic Debris Avalanche Transport and Emplacement Mechanisms,the base, bulldozing and incorporation of substrata change the composition and behaviour of the VDA. In extreme cases, VDAs transform into lahars if sufficient water is available for entrainment. Post-emplacement, lahars can also happen, e.g., through debris dewatering, loading of saturated substrat

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Sedimentology of Volcanic Debris Avalanche Deposits,ifferent origin show that preservation of source stratigraphy, (mega-)clasts, jigsaw-fractured clasts, and incorporation of runout path material are common features. Their unique composition, grain sizes, and abundance of matrix sets VDADs apart from deposits of large rockslides and debris flows. Th