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Alluvial fans

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Encyclopedia of Sediments and Sedimentary Rocks

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Introduction

Alluvial fans are depositional features, formed of coarse gravel sediments, created where high-bed-load streams enter zones of reduced stream power, and deposit the coarser fraction of their loads. The resultant landforms are usually fan-shaped in plan and wedge-shaped in profile (Bull, 1977). They occur commonly in two topographic situations: at mountain fronts and at tributary junctions (Harvey, 1997). They are subaerial features, however if they extend into water they are known as fan-deltas.

Sediment transport and deposition processes on alluvial fans range from debris flows, to sheetfloods and channelized streamflows. Fans range in axial length up to 10s of km, though many fans described in the literature range in size between ca. 100 m and a few km. As scale increases there is a tendency for the dominant process to change, from small debris-flow dominated tributary-junction fans (debris cones), to mixed processes and sheetflood dominance at intermediate scales, and...

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Harvey, A.M. (1978). Alluvial fans. In: Middleton, G.V., Church, M.J., Coniglio, M., Hardie, L.A., Longstaffe, F.J. (eds) Encyclopedia of Sediments and Sedimentary Rocks. Encyclopedia of Earth Sciences Series. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-3609-5_3

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  • DOI: https://doi.org/10.1007/978-1-4020-3609-5_3

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