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- W2040281978 abstract "Abstract The Campine Plateau in northeastern Belgium, a remnant of an alluvial fan deposited by the Meuse River during the mid-Pleistocene, is characterised by the presence of boulders with maximum dimensions of up to 2 m, embedded in a gravel matrix. These boulders originated in the Ardennes region and are generally assumed to have been transported by ice-rafting processes. This paper investigates for the first time quantitatively the possibility of purely hydraulic transport of the boulders, taking into account channel and flow characteristics in the boulder provenance area during the mid-Pleistocene. Empirical transport relations that describe incipient motion thresholds in nonuniform river beds as a function of the relative grain size, or the ratio between the grain size of interest and the median grain size of the channel bed, are applied in order to calculate critical water depths for transport of boulders of various sizes. Results indicate that hydraulic transport of boulders with intermediate diameters" @default.
- W2040281978 created "2016-06-24" @default.
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- W2040281978 date "2015-01-01" @default.
- W2040281978 modified "2023-09-27" @default.
- W2040281978 title "What was the transport mode of large boulders in the Campine Plateau and the lower Meuse valley during the mid-Pleistocene?" @default.
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- W2040281978 doi "https://doi.org/10.1016/j.geomorph.2014.10.010" @default.
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