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193 Table 2 Simplified example of scale of hazard based on vegetation types for the Central Alps area . . .. . . . . . . . . . 199 xxxi xxxii List of Tables Using Age of Colonizing Douglas-Fir for the Dating of Young Geomorphic Surfaces—A Case Study . . . . . . . . . . .. . . . . . . . . . 203 Table 1 Summary of mean values for breast height growth time (BHGT), germination lag time (GLT) and colonization time gap (CTG) for all study sites . .

In: Rachocki AH, Church M (eds) Alluvial fans: a field approach. Wiley, Chichester, pp 69–89 Blair TC, McPherson JG (1994) Alluvial fan processes and forms. In: Abrahams AD, Parsons AJ (eds) Geomorphology of desert environments. Chapman & Hall, London, pp 354–402 Blair TC, McPherson JG (2009) Processes and forms of alluvial fans. In: Parsons AJ, Abrahams AD (eds) Geomorphology of desert environments, 2nd edn. Springer, New York, pp 413–467 Bloetzer W, Egli T, Petrascheck A, Sauter J, Stoffel M (1998) Klima¨anderungen und Naturgefahren in der Raumplanung – Methodische Ans¨atze und Fallbeispiele.

These ‘preparatory’ processes include rockfall, snow avalanche, debris-flow, and fluvial processes such as sheet flood and channelized stream flow (Blair and McPherson 1994; Harvey 2012, this volume). The supply of sediment to fans and cones is not continuous but almost always episodic and generally related to major rain- and hailstorms. g. through defects in water conduits, tubes). Catchment size is a critical parameter for the generation of hydrogeomorphic processes and influences flood magnitude.

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Aging Assessment - Westinghouse PWR, GE BWR Containment Isol Fns

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