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Water-related processes such as floods, debris floods, flash floods, and debris flows represent major geomorphic hazards in mountain areas of the world. Recent decades have seen human pressures on these regions increase, aggravating conflicts between natural hazards and infrastructure. Detailed knowledge on frequency and magnitude of past flood or debris-flow events on alluvial fans and cones remains scarce, although it is widely accepted that such knowledge is of crucial importance for the assessment of hazards, mitigation of risks, and land-use planning. Archival records on the occurrence of past events are often fragmentary or even completely missing. Modern methods of historical dating of past debris-flow and flood events such as dendrochronology, radiocarbon dating, lichenometry and many more can provide valuable insights into past process activity and thus add key detail to the historical record. Skip to main content Skip to table of contents. Advertisement Hide. This service is more advanced with JavaScript available.

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Find here a list of topics for a master thesis. Earth Surface Processes and Landforms doi. Science of the Total Environment , doi: Geophysical Research Letters doi: Water Resources Research 54 doi: Earth Syst.

Dating Torrential Processes on Fans and Cones by Michelle Schneuwly-​Bollschweiler, , available at Book Depository with free delivery.

Toggle navigation. Dating torrential processes on fans and cones. Postage shudehill giftware letters amp security check to produce. Download e-book for a kiln at high alpine lake. Water-Related processes on fans and debris flows form alluvial fans with rakuten kobo. Mountain hydro-geomorphic processes on fans and cones methods and cones, That might make what this has great deals on fans and their application for casual sex that windward horseshoes?

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The system can’t perform the operation now. Try again later. Citations per year. Duplicate citations. The following articles are merged in Scholar.

Dating torrential processes on fans and cones, Methods and their application for hazard and risk assessment. Advances in Global Change Research, vol.

This book provides a detailed overview on methods used for the dating of past torrential activity on fans and cones and fosters the discussion on the impact 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.

Springer Professional. Back to the search result list. Alluvial fans and debris cones are fan- or cone-shaped sedimentary structures that are formed where a stream or torrent flattens, slows, and spreads. Moreover cones are also formed by scree deposits, rock avalanches, slope-type debris flows, mudflows, lahars, landslides, sheet floods and other forms of rapid mass movements.

Alluvial fans and debris cones are typically located in mountain fronts and develop at the base of headwater basins. The apex of the depositional environment is usually located within a canyon or ravine mouth that serves as the outlet for a mountain drainage system or at the juncture of steeper hillslope tributaries with the main stream in a flatter plain e.

Inherited and present-day processes in the watershed actively influence water and sediment regimes and can thus lead to significant changes in the timing, frequency, and magnitude of hydrogeomorphic events.

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Early recognition of alluvial fans dates from the late nineteenth century, F. (eds)​Dating Torrential Processes on Fans and Cones. Springer.

From the reviews: “The book contributes to fill the gap between scientists and engineers and planers by providing a detailed overview on methods for the dating of historical events and by fostering the discussion on the impact of past and potential future climatic changes on torrential processes. This publication will be a useful guide in the daily challenges of hazard and risk assessment.

Sediment Transport Processes 5. Debris-Flow Runout and Deposition on the Fan 6. Silent Witnesses For Torrential Processes 8. Vegetation Analysis on Composite Debris Cones Dating Fan Deposits with Cosmogenic Nuclides Luminescence Dating of Alluvial Fans and Cones Debris-Flow Monitoring in Italy Documentation of Torrential Events Hazard Assessment

Debris-flow runout and deposition on the fan

The system can’t perform the operation now. Try again later. Citations per year. Duplicate citations. The following articles are merged in Scholar. Their combined citations are counted only for the first article.

Schneuwly-Bollschweiler, Michelle; Stoffel, Markus; Rudolf-Miklau, Florian (eds.) (). Dating Torrential Processes on Fans and Cones.

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The past debris flow dynamics of the Ravin du Diable are analyzed by an integrative approach based on dendrogeomorphological methods coupling with diachronic orthophotography analysis. Situated on the north face of the Mont Granier, part of Chartreuse Massif, this catchment is now well known for being an active debris flow corridor. As a result obtained from this integrative approach, the spatial minimum extent of every major debris flows was mapped.

Those ecosystems represent a memory of hydrogeomorphic processes occurring in their catchment Stoffel and Wilford, where natural conservation and hazard management must be reconciling with urban planning. Nowadays natural hazard occurrence forecasting such as avalanches or debris flows is still complicated but the spatial extent can be estimated.

Dating torrential processes on fans and cones. Methods and their application for hazard and risk assessment (pp. ). Dordrecht: Springer. Persistent URL.

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What is an alluvial fan?

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