Titlebook: Landforms of the World with Google Earth; Understanding our En Anja M. Scheffers,Simon M. May,Dieter H. Kelletat Book 2015 Springer Science

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Tectonic Landformsmazing patterns of folds, faults or fractures? Early geologists who understood all too well that most sedimentary rocks had been laid down as soft, horizontal layers have wrestled with questions such as these for centuries. Most educated Europeans during the medieval age until the 1700s were convinc

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Karst Landscapes: Topographies Sculptured by Dissolution of Rocky dissolved and weathered materials. The development of all karst landforms requires the presence of rock types capable of being dissolved by surface water or ground water. Throughout the world, karst landscapes vary from rolling hills dotted with sinkholes to jagged hills, pinnacle karst and tower

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Mass Movements: Landforms Shaped Under the Force of Gravityudent of the institution and his colleagues put Einstein’s general theory of relativity to the test in a cosmic laboratory 7,000 light years from Earth, where two exotic stars – a pulsar or neutron star and a white-dwarf – are circling each other. Einstein’s theory states that objects with mass caus

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Planar Forms and Plain Forming Processes: Pediments/Glacis, and Peneplains (with Inselbergs)to form (millions or tens of millions of years). Nevertheless, there are typical planar forms according to climate provinces like the glacis or pediments in arid and semi-arid environments along the feet of mountains or mountain chains. The largest planar forms and the oldest ones are the peneplains

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Forms by Wind (or: Aeolian Processes): Deflation and Dunescapes and the generation of landforms. While this idea may be true for the destructive aeolian process of deflation and its resulting landforms, the depositional aeolian processes such as dune formation are responsible for a remarkable variety of important (large and small) landforms that characteri