Geography of Lesotho rises in the Drakensberg mountains in northeastern Lesotho and flows across the entire length of the country before exiting to South Africa at the Mohale's Hoek District in the southwest. The Caledon River marks the northwestern part of the border with South Africa. Other rivers include the Malibamatso, Matsoku and Senqunyane. The bedrock of Lesotho belongs to the Karoo Supergroup, consisting mostly of shale and sandstone. Peatlands can be found in the highlands of Lesotho, most extensively in the mountainous escarpment near the country's eastern border. The summit of Thabana Ntlenyana is partially encircled by bogs. Solifluction deposits, blockfields, blockstreams
History of Lesotho head of the army, the Prime Minister fled the country alleging a coup was taking place. Kamoli denied that any coup had occurred. History of Lesotho The history of people living in the area now known as Lesotho () goes back as many as 40,000 years. The present Lesotho (then called Basutoland) emerged as a single polity under paramount chief Moshoeshoe I in 1822. Under Moshoeshoe I, Basutoland joined other tribes in their struggle against the Lifaqane associated with the reign of Shaka Zulu from 1818 to 1828. Subsequent evolution of the state was shaped by contact with the British