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The Marungu highlands are in the Katanga Province of the Democratic Republic of the Congo, to the west of the southern half of Lake Tanganyika. ==Location== The highlands are divided by the Mulobozi River, which flow into the lake just north of Moba port. The northern section reaches an altitude of while the larger southern part reaches . Mean annual rainfall is around , mostly falling between October and April. The soil is relatively low in nutrients. A sublacustrine swell extends from the Marungu plateau under the southern basin of Lake Tanganyika, subdividing it into the Albertville and Zongwe basins. The Zongwe trough holds the deepest part of the lake, at below the present lake level. Alluvial cones from the rivers that drain the Marungu Plateau are present in the foot of the Zongwe trough, and there are many V-shaped valleys below the lake level. These features indicate that during the Quaternary (2.588 million years ago to the present) the lake level has varied greatly, at times being much lower than is now. The explorer Henry Morton Stanley noted this feature when he visited the region in his journey of 1874–77. He wrote, "Kirungwé Point appears to be a lofty swelling ridge, cut straight through to an unknown depth. There seems ground for believing that this ridge was once a prolongation of the plateau of Marungu, as the rocks are of the same material, and both sides of the lake show similar results of a sudden subsidence without disturbance of the strata." 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Marungu highlands」の詳細全文を読む スポンサード リンク
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