Deserts and glacial landscapes argon truly much opposites. The desert landscapes be mainly bring to passd by thread and smoothen, but they are defined by the regions annual rainfall. The landscapes of the desert are composed of sand, alluvial fans, playas, oases, arroyos, as well as deposits of salt. Wind eroding, or eolian, is the type of erosion which is seen in the desert. The direction of the wind is constantly changing and transforming the desert. An congressman of a feature in a desert landscape that is noticeable would be the dunes. Dunes are hills, or ridges, of sand that are created when the wind blows. There are five different types of these mounds of sand although they are irregular. They are barchans, transverse, star, parabolic, and longitudinal. Desertification, or the movement of desert conditions into non-desert regions analogous in Northern China, is one way that deserts are formed.
With areas like that of Northern China in a beautiful balancing act to maintain its ecosystem, even minor stresses by human (anthropogenic) or natural forces can become similarly much to tolerate, thus a degradation of the land results. virtually desert lands arent covered by sand. Water erosion is an important geologic process in deserts. Flash floods create deep canyons called arroyos and create depositional landforms such as alluvial fans. This blood that deserts have with water makes deserts comparable to glacial landscapes because glacial landscapes are mainly formed by water.
hike up and retreat is a huge factor in the base of glaciers. Ultimately formed by receding water from glaciers, this landscape can have any number of...If you want to scotch a full essay, order it on our website: Orderessay
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