Titlebook: Dating Torrential Processes on Fans and Cones; Methods and Their Ap Michelle Schneuwly-Bollschweiler,Markus Stoffel,Fl Book 2013 Springer S

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Using Age of Colonizing Douglas-Fir for the Dating of Young Geomorphic Surfaces—A Case Studylains, etc.) for purposes of hazard assessment and mitigation commonly requires greater dating precision than is available through radiocarbon dating or other methods. Ages of trees growing on landform surfaces have been used in a number of studies to estimate the time of landform creation or surfac

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Radiocarbon Dating: Alluvial Fan/Debris Cone Evolution and Hazardstial. This development mirrors the contributions made in investigations of other depositional environments since invention of the technique in the 1950s (Cook and van der Plicht 2007; Jull 2007). Radiocarbon dating involves measuring the amount of the radioisotope .C preserved in fossil organic mate

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Book 2013impact of past and potential future climate change on torrential processes. The book has a clear focus on the practical applications of these methods, complemented by case studies. The limits of each dating method in case of excessive natural and human interventions on fans and cones are shown.

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Processes of Sediment Supply to Alluvial Fans and Debris Conesl fans”. Such landforms are found in three main settings (Harvey 2010): mountain-front, intra-montane, and tributary-junction settings. They occur in all climatic environments, but again, within the context of this book the focus is on dry-region, and temperate upland and mountain environments.

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Susceptibility and Triggers for Debris Flows: Emergence, Loading, Release and Entrainment in size from clay to boulders, and may contain a large amount of woody debris. Volumes of material delivered by single events vary from less than 100 to more than 100,000m.. Generally three factors are necessary for a debris flow to develop: water, sufficient inclination, and abundant sediment supply.

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https://doi.org/10.1007/978-3-319-67765-1f rock walls following deglaciation, and the severity of the climate (Matsuoka and Sakai 1999; Ballantyne 2002; Curry and Morris 2004). These factors are conducive to the development of fan deposits by rockfall, debris-flow and avalanche activity, each of which represent a significant hazards to fan areas.

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