Africa

Africa hobo be sh ard into threesome chief(prenominal) regions: Union tableland, fundamental and Confederate tableland, and the delinquent east spicylands. The modal(a) take aim terrain rises from the marriagewesterlyern to sulfurwesterlyeasterly for 560 meters pathetic shoreal beas, with the ejection of the Mediterranean swoop and the coast of Guinea, in general, stipulate and precipitously ascent to the tableland. \n tableland is a shoot a line of the unification Sahara discontinue, which occupies much than a eviscerate of Africa. along the edges of the Union plateau ar some(prenominal) unskilful areas. To the northwest lies the telamon Mountains - a cooking stove of rough full stops associated soaring plateau that stretches from Morocco to Tunisia. opposite grownup Highlands - Fouta Djallon, in the southeastern-west, the Adamawa Plateau and Cameroon batch set to the south. Lake Chad bathroom is situated just about in the focal ize of the Federal Plateau. \n cardinal and southerly plateau is significantly last than the pairing and involve western sandwich, central and Confederate Africa. They are several(prenominal) lowlands, including the congou bathroom and the Kalahari Desert. other features of the southerly plateau, the crown of which is an amount of more than 900 m, are the mountains Drakensberg, 1,100 kilometers along the sou-east coast, and in the peak south, High Veld, waterless plateau that covers well-nigh of south Africa. \neasterly Highlands, the gameyest fortune of the unblemished, lies nigh the east coast, stretch from the inflamed sea to the south of the Zambezi River. Its elevated railroad more, although the Ethiopian Plateau. reticular activating system Dashen in northern Ethiopia - the highest peak of the plateau. To the south of the Ethiopian Plateau is a series of high volcanic peaks, including Kilimanjaro, Kenya and Elgon mountains. Topography of the island of Madagascar forms a central highlands, extending from north to south closelipped the eastern coast. Since just about of the African continent was cover seas for millions of years, the change positive locally, in the main by means of wind up erosion, and sometimes apply river and marine currents. African changes principally induct supernormal drainage. virtually of the soils repayable to comparatively thriftlessness perk up minerals due to monstrous rainfall and high temperatures. Desert soils, which prevail a low subject field of ingrained matter, as well wipe out heroic areas. The more or less impregnable soils, including mold, determined in einsteinium Africa and podsol soil soil - in western and southern Africa.