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Field investigation of valley bottoms of underflt streams by means of augering or of seismic refraction demonstrates large channels that meander around valley bends. Information from miscellaneous sources that is, civil-engineering records from damsites supplements and confirms the writer's findings. The large channels are taken as the beds of former large streams; their infilling is ascribed to stream shrinkage rather than to aggradation.
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G. H. Dury (1964) studied this question.
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