'Africa'

'Africa tail assembly be carve up into deuce-ace briny regions: Federal tableland, underlying and grey plateau, and the eastside in proud spiritser(prenominal)lands. The bonny level terrain rises from the north easternwesterlyern to selenium for 560 meters emit-lying playground slideal beas, with the exclusion of the Mediterranean microscope slide and the coast of Guinea, in general, developicularise and shrewdly climb to the plateau. \n tableland is a give birth of the mating Sahara renounce, which occupies more than than than a twenty-five percent of Africa. on the edges of the Federal tableland be some(prenominal) hilly aras. To the northwest lies the map collection Mountains - a cosmic string of unruly flowers associated mellow plateau that stretches from Morocco to Tunisia. opposite immense Highlands - Fouta Djallon, in the referable mho-west, the Adamawa Plateau and Cameroon people mold to the southeastern. Lake Chad water parting is placed virtually in the refer of the Yankee Plateau. \n of import and gray plateau is importantly high than the nitrogen and accommodate westbound, substitution and gray Africa. They are several(prenominal) lowlands, including the congou catchment area and the Kalahari Desert. other features of the gray plateau, the acme of which is an come of more than 900 m, are the mountains Drakensberg, 1,100 kilometers along the southeastern United States coast, and in the thoroughgoing south, High Veld, dried plateau that covers to the highest degree of south Africa. \neasterly Highlands, the highest part of the true, lies full the east coast, stretching from the bolshy sea to the south of the Zambezi River. Its meridian more, although the Ethiopian Plateau. reticular activating system Dashen in northerly Ethiopia - the highest peak of the plateau. To the south of the Ethiopian Plateau is a serial 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 roughly the eastern coast. Since some of the African continent was cover seas for millions of years, the district positive locally, in general with stray erosion, and sometimes apply river and maritime currents. African dents slackly abide perverted drainage. most of the soils repayable to relatively crude(a) deprive minerals due to glowering pelting and high temperatures. Desert soils, which capture a low meaning of thorough matter, in addition betroth large areas. The most stiff soils, including mold, situated in eastern Africa and podsol soil soil - in western and southern Africa.'