Titlebook: Landforms of the Earth; An Illustrated Guide Francisco Gutiérrez,Mateo Gutiérrez Book 2016 Springer International Publishing Switzerland 20

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Karst Landforms,inage network is typically absent or deranged, and it flows rapidly in the subsurface through conduit networks and caves towards springs. Three main types of karst settings can be differentiated: bare karst, covered or mantled karst and interstratal karst, depending, respectively, on whether the sol

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Weathering Landforms,, weathering by dissolution is the dominant morphogenetic process. Weathering processes are typically classified into physical, chemical and biological, although there are frequently some overlaps and interrelationships. Moreover, a significant number of similar weathering landforms may be produced

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Slope Movements,e limited by flank collapses that can drastically change the behaviour of volcanic eruptions. Landslides are very common in the seafloor, especially on the continental slope, and include the largest mass movements on Earth, reaching volumes of the order of 10. m.. Some of the main triggers for terre

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Desert and Aeolian Landforms,ution of stable high-pressure cells in the subtropics (e.g. Sahara and Arabian deserts); (2) the continentality, based on the distance to the oceans that constitute the main source of moisture (e.g. deserts in Central Asia); (3) orographic barriers that block the path of weather fronts creating rain

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Book 2016t to know about the terminology and origin of the landforms they encounter in their trips. In many cases, the geomorphological features constitute the main asset of first-class protected areas (e.g., UNESCO World Heritage Sites, National Parks).