Titlebook: Rivers and River Terraces; G. H. Dury Book 1970 Palgrave Macmillan, a division of Macmillan Publishers Limited 1970 geography.physical geo

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一美元

Introduction,ticle or a dissertation. This would have been to defeat the central purpose of assembling original material from a variety of sources, and of presenting it in conveniently abbreviated form but still at significant length.

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River Channel Patterns,cussed, there is a gradual merging of one pattern into another. The difference between a sinuous course and a meandering one is a matter of degree. Similarly, there is a gradation between the occurrence of scattered islands and a truly braided pattern.

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伪善

Longitudinal Profiles of the Upper Towy Drainage System,eastwards, ultimately reaching the Bristol Channel; others, such as the Rheidol and the Ystwyth, flow westwards across the Coastal Plateau into Cardigan Bay. The Teifi, which reaches that bay much farther south, lies mainly on the Lower Plateau, its course being for some distance almost parallel to

Preserve

Land Sculpture in the Henry Mountains, principles of earth sculpture, and its resources are far from exhausted. The following account, based principally on research in the Henry Mountains, restates certain principles of erosion which have been derived from, or confirmed by, work in the Colorado Plateau country.

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Erosional Development of Streams: Quantitative Physiographic Factors,ns are described as youthful, mature, old, poorly drained or well drained, without specific information as to how, how much or why. An effort will be made in the present paper to show how the problem of erosional morphology may be approached quantitatively. Drainage-basin development by ground-water

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得意人

River Channel Patterns,e channel of a great river are the same as those operating in a small one. One step towards understanding the mechanisms of operation is to describe many rivers of various kinds. The present study is concerned principally with channel pattern. The term refers to limited reaches of channel that can b