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Auteur L. Leopold |
Documents disponibles écrits par cet auteur (7)
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This book deals primarily with landform development under processes associated with running water. In part I, the relation of geomorphology to field problems is analyzed in studies of a mountain block in a semiarid climate, a meandering river cu[...]ouvrage
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Bankfull discharge is important because the bankfull stage is the level at which water begins to flow over the floodplain. When water flows over the floodplain, then it is by definition a flood. Bankfull discharge is also important because of it[...]rapport
L. Leopold ; M. Wolman ; US GEOLOGICAL SURVEY | Washington [USA] : US Government Printing Office | Geological survey professional paper 282-B | 1957Channel pattern is used to describe the plan view of a reach of river as seen from an airplane, and includes meandering, braiding, or relatively straight channels. Natural channels characteristically e.ools or deep reaches and riffles or shallow[...]rapport
M. Wolman ; L. Leopold ; US GEOLOGICAL SURVEY | Washington [USA] : US Government Printing Office | Geological survey professional paper 282-C | 1957On many small rivers and most great rivers, the flood plain consists of channel and overbank deposits. The proportion of the latter is generally veryu small. Frequency studies indicate that the flood-plain surface and the small amount of deposit[...]ouvrage
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L. Leopold ; T. Madock ; UNITED STATES GEOLOGICAL SURVEY | Washington, USA : United States Government Printing Office | Geological survey professional paper 252 | 1953Quantitative measurement of some of hydraulic factors that help to determine the shape of natural stream channels : depth, width, velocity, and suspended load, and hw they vary with discharge as simple power functions. Their interrelations are d[...]