Titlebook: Geomorphology of Desert Environments; Athol D. Abrahams,Anthony J. Parsons Book 19941st edition Athol D. Abrahams and Anthony J. Parsons 1

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https://doi.org/10.1007/978-3-642-79069-0parseness of vegetation, results in more widespread occurrence of slopes with little or no regolith than in areas with humid climates. This chapter outlines the processes and landforms occurring on desert slopes that are either massive bedrock or are scarps and cuestas in layered rocks dominated by

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https://doi.org/10.1007/978-3-319-30012-2hich are dealt with in Chapters 13 and 14) nor are developed in highly erodible, fine-grained sedimentary rocks (i.e. badlands slopes, which are treated in Chapter 9). Such hillslopes in desert (arid and semi-arid) climates are usually mantled with a thin layer of coarse debris that has either weath

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https://doi.org/10.1007/978-1-4684-1755-5 are fluvial and aeolian, which operate on a surface with a very reduced vegetation cover. Indeed vegetation is absent in many areas. Even in more favourable locations plant cover may not reach 50%, giving an impression of the predominance of bare ground. Biogenic processes affecting landform evolut

maintenance

Masanori Uchikawa,Tatsuya Takemotothat exist; secondly, as a chemical substance which interacts with other chemical substances, notably salts; third, as a medium of transport of mass; and, fourth, as a direct source of energy. The last role, though small by comparison with the roles of solar and wind energy, may none the less be cri

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Petra Sim?i?,Alessio Pierini,George Lubas-arid areas. This is due largely to the originality, forcefulness, and intellectual background of American geomorphologists developed during and sustained long after the exploration of the American West. The strong sense of field observation and experiment coupled with a deep historical perspective,

Concrete

Electroslag Remelting Towards Clean Steelings. Reported on six continents, their distribution spans the range of subpolar latitudes from the Arctic to the Antarctic and the range of climate from hyperarid to humid tropical (Whitaker 1979). On the Cape York Peninsula in tropical north-east Queensland, a tecto-nically quiescent region of Pre

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HAUNT

Overview: Over the last twenty years there has been a major expansion ofknowledge in the field of landforms and landforming processes ofdeserts. This advanced-level book provides a benchmark for thecurrent state of science, and is written by an international team ofauthors who are acknowledged experts in their fields.978-94-015-8254-4