Titlebook: Climatic Geomorphology; Edward Derbyshire Textbook 1973Latest edition Macmillan Publishers Limited 1973 geography.Geomorphology.linguistic

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书目名称Climatic Geomorphology影响因子(影响力)




书目名称Climatic Geomorphology影响因子(影响力)学科排名




书目名称Climatic Geomorphology网络公开度




书目名称Climatic Geomorphology网络公开度学科排名




书目名称Climatic Geomorphology被引频次




书目名称Climatic Geomorphology被引频次学科排名




书目名称Climatic Geomorphology年度引用




书目名称Climatic Geomorphology年度引用学科排名




书目名称Climatic Geomorphology读者反馈




书目名称Climatic Geomorphology读者反馈学科排名

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The Geographical Cycle, structure, process, and time. In the beginning, when the forces of deformation and uplift determine the structure and attitude of a region, the form of its surface is in sympathy with its internal arrangement, and its height depends on the amount of uplift that it has suffered. If its rocks were un

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The Cycle of Glaciation,factor of supreme importance is temperature, a very moderate change in the average annual temperature being sufficient to transform a temperate district completely, and to furnish it with snowfields and mountain glaciers.

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Morphology of Climatic Zones or Morphology of Landscape Belts?,h was divided into morphoclimatic zones, and the surface landforms of each area were discussed. While climatic zones are usually delineated on the basis of average values of precipitation, temperatures and humidity, it is to be expected that any attempt to delineate ‘morphological climatic zones’ wi

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Landforms of the Savanna Zone with a Short Dry Season,e, the dry season lasts for such a time that the characteristic features of a dry climate are so clearly developed that they become morphologically important. In the dry season rain must entirely cease and the temperatures must be so high that the ground really dries out, high enough, in fact, to ca

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The Problem of Erosion Surfaces, Cycles of Erosion and Climatic Geomorphology,orms a fascinating and stimulating basic idea. It is true that objections have been raised, particularly in Germany, against Davis’s views. A. Hettner (1921) and S. Passarge (1912), in particular, have pointed out several uncertainties in Davis’s deduction and stress the necessity for a more thoroug

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The Theory of Savanna Planation,introduced in an attempt to explain its origin (Cotton, 1942(a)). This landscape type, which is common in the tropics, is characterised by a great extent of very smooth, nearly level plains which are flooded in the wet season. From the plains inselbergs rise abruptly, forming very steep-sided isolat

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