By Andrew S. Goudie
According to 4 a long time of study by way of Professor Andrew Goudie, this quantity offers a state of the art synthesis of our knowing of wasteland geomorphology. It offers a really overseas point of view, with examples from worldwide. largely referenced and illustrated, it covers such issues because the value of prior climatic alterations, the variety of alternative barren region environments, rock breakdown, wind erosion and dirt typhoon new release, sand dunes, fluvial and slope kinds and procedures, the function of the utilized geomorphologist in wilderness improvement and conservation, and the Earth as an analogue for different planetary our bodies. This e-book is destined to turn into the vintage quantity on arid and semi-arid geomorphology for complicated scholars and researchers in actual geography, geomorphology, Earth technology, sedimentology, environmental technology, and archaeology.
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Additional resources for Arid and Semi-Arid Geomorphology
10 The Geography and Frequency of Change In a mid-latitude location like the south-west region of the United States (Smith and Street-Perrott, 1983), there was greatly increased effective moisture at the time of the LGM. 10 The Geography and Frequency of Change 29 associated rain-bearing depressions, particularly in winter. 9. , 2012). The tropics were much less influenced by the displaced full glacial westerlies than mid-latitudes. They experienced relatively dry conditions at that time but subsequently experienced a major pluvial in the early to mid-Holocene (Grove and Goudie, 1971).
G. , 2009). 5) owe much to the opening of the South Atlantic by sea-floor spreading in the late Jurassic and early Cretaceous as well as the presence of the great hotspot associated with the Walvis Ridge (Goudie and Eckardt, 1999). 6) are associated with passive-margin evolution. 7), features such as the Red Sea rift, the Dead Sea transform fault, the Zagros Mountains and the ophiolitic ranges of Oman result from being at a crossroads of major plate boundaries (Guba and Glennie, 1998). 10). 14) is a low, dry, ancient continent with a long history of comparative orogenic stability over large areas, so that many of the present landscape features are inherited from a great variety of climates that may go back to the Jurassic or earlier (Twidale, 2000).
The flow of rivers showed great variability during the Quaternary. , 2010). Indeed, sapropel (organic-rich mud) layers in the eastern Mediterranean give a good picture of Nile flow variability in the late Pleistocene. , 2004). , 2003). Ethiopian rivers, fed by strong monsoon rains in summer, caused a strong seasonal flood in the Nile, and eleven sapropel events have taken place during the last 465,000 years. 9 Lakes of the Quaternary Deserts have many types of lake basin. 10), and so forth. They have a multitude or origins, including deflation, solution of limestone (as in the case of dayas) and evaporites, meteorite impact, aeolian blocking of drainage and tectonic subsidence.