Fig. 6.22. Photograph of a section in a wadi in the Sarir Calanscio, eastern Libya. This shows the lag gravel
of a sarir surface developed on a poorly sorted Pleistocene alluvial fan deposit. The gravel surface prevents
further eolian deflation.
Fig. 6.23. Large-scale cross-bedding in Permian red sands of presumed eolian origin. Dawlish, southwest
England.
of a sarir surface developed on a poorly sorted Pleistocene alluvial fan deposit. The gravel surface prevents
further eolian deflation.
Fig. 6.23. Large-scale cross-bedding in Permian red sands of presumed eolian origin. Dawlish, southwest
England.