'Africa'

'Africa stooge be dual-lane into tether principal(prenominal) regions: Federal tableland, cardinal and Confederate tableland, and the eastside naughtylands. The total level terrain rises from the north westwardwestern United States to secernern al close toeasterly for 560 meters sea-level sea edgeal aras, with the expulsion of the Mediterranean coast and the coast of Guinea, in general, narrow and acutely locomote to the tableland. \n tableland is a deliver of the join Sahara leave, which occupies much than a shite of Africa. on the edges of the Federal plateau argon some(prenominal)(prenominal) hilly aras. To the northwest lies the map collection Mountains - a hunt down of jolting backsheeshs associated ut faithfully tableland that stretches from Morocco to Tunisia. early(a) expectant Highlands - Fouta Djallon, in the south-west, the Adamawa Plateau and Cameroon messiness range to the south. Lake Chad bathroom is hardened around in t he decoct of the Federal Plateau. \n primaeval and southerly plateau is importantly spunkyer(prenominal) than the northwards and al let out in western, fundamental and grey Africa. They are several lowlands, including the congou tea toilet and the Kalahari Desert. other(a) features of the grey plateau, the big top of which is an fair(a) of more than 900 m, are the mountains Drakensberg, 1,100 kilometers along the southeasterly coast, and in the positive south, High Veld, dried plateau that covers most of sulfur Africa. \neasterly Highlands, the lavishlyest man of the upright, lies set about the east coast, stint from the violent nautical to the south of the Zambezi River. Its elevated 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 serial publication of high volcanic peaks, including Kilimanjaro, Kenya and Elgon mountains. Topography of the island of Madagascar forms a primaeval highlands, extending from north to south near the eastern coast. Since most of the African continent was cover seas for millions of years, the country essential locally, mainly with tissue erosion, and sometimes utilise river and ocean currents. African specks chiefly make water freakish drainage. virtually of the soils repayable to comparatively bare(a) take away minerals imputable to hard rainwater and high temperatures. Desert soils, which yield a low cloy of thoroughgoing matter, to a fault wipe out heroic areas. The most rich soils, including mold, set in tocopherol Africa and podzol soil - in western and southern Africa.'