Drakensberg in the context of "Sotho language"

The Maloti Mountains are a mountain range of the highlands of the Kingdom of Lesotho. They extend for about 100 km into the South African Free State. The Maloti Range is part of the Drakensberg system that includes ranges across large areas of South Africa. "Maloti" is also the plural for Loti, the currency of the Kingdom of Lesotho. The range forms the northern portion of the boundary between the Butha-Buthe District in Lesotho and South Africa's Free State.

Aloe polyphylla, the spiral aloe, kroonaalwyn, lekhala kharetsa, or many-leaved aloe, is a species of flowering plant in the genus Aloe that is endemic to the Kingdom of Lesotho in the Drakensberg mountains. An evergreen succulent perennial, it is well known for its strikingly symmetrical, five-pointed spiral growth habit.

Mokhotlong is a constituency, city and seat of Mokhotlong District in the mountainous northeastern part of Lesotho. It is the first major city with an airport along the road from South Africa across the Sani Pass, near the Maloti (Drakensberg in South Africa) Mountains. The name of the city is named in Sesotho, the language of the people of Lesotho, meaning "Place of the Bald Ibis." Thabana Ntlenyana, the highest point in southern Africa, is found in Mokhotlong.

The Lesotho Highlands are formed by the Drakensberg and Maloti mountain ranges in the east and central parts of the country of Lesotho. Foothills form a divide between the lowlands and the highlands. Snow is common in the highlands in the winter.

The Caledon River (Sotho: Mohokare) is a major river located in central South Africa. Its total length is 642 km (399 mi), rising in the Drakensberg Mountains on the Lesotho border, flowing southwestward and then westward before joining the Orange River near Bethulie in the southern Free State. The river was originally named Prinses Wilhelminas Rivier in 1777, by Colonel R J Gordon.

The border between Lesotho and South Africa is 909 kilometres (565 mi) long and forms a complete loop, as Lesotho is an enclave entirely surrounded by South Africa. The border follows the Caledon River, the drainage divide of the Drakensberg mountains, the Orange River, the Makhaleng River, and a series of hills joining the Makhaleng back to the Caledon.

Msunduzi Municipality (Zulu: UMasipala wase Msunduzi) is a local municipality within the Umgungundlovu District Municipality, in the KwaZulu-Natal province of South Africa. It encompasses the city of Pietermaritzburg, which is the capital of KwaZulu-Natal and the main economic hub of the Umgungundlovu District Municipality.

Msunduzi Municipality is situated on the N3 highway at a junction of an industrial corridor (from Durban to Pietermaritzburg) and an agro-industrial corridor (stretching from Pietermaritzburg to Estcourt). On the regional scale, it is located at the cross section of the N3 corridor and the Greytown Road corridor to the north, a tourist route to the Drakensberg, and Kokstad Road to the south.

The Cape Fold Belt (CFB) is a 1,300 kilometres (810 mi) long fold-and-thrust mountain belt along the western and southern coastlines of Western Cape, South Africa. The Cape Fold Belt formed during the Permian period (300 to 250 million years ago) in the late Paleozoic age, affecting the sequence of sedimentary rock layers of the siliciclastic Cape Supergroup with folding and faulted rocks, which were deposited in the Cape Basin in the southwestern corner of South Africa.

The Cape Fold Belt was once part of a larger orogenic belt with other mountain ranges that formed as part of the same tectonic event that originally extended from Argentina, across southern Africa, and into Antarctica. It included the Ventana Mountains near Bahía Blanca in Argentina, the Pensacola Mountains in East Antarctica, the Ellsworth Mountains in West Antarctica, and the Hunter–Bowen orogeny in eastern Australia. The rocks involved in this fold system are primarily sandstones and shales, with shales from the Bokkeveld Group persisting in valley floors, while the more erosion-resistant sandstones of the Peninsula Formation form the parallel ranges of the Cape Fold Mountains. The highest peak in the range is Seweweekspoortpiek, which reaches 2,325 meters.

The Karoo Supergroup is the most widespread stratigraphic unit in Africa south of the Kalahari Desert. The supergroup consists of a sequence of units, mostly of nonmarine origin, deposited between the Late Carboniferous and Early Jurassic, a period of about 120 million years.

In southern Africa, rocks of the Karoo Supergroup cover almost two thirds of the present land surface, making part of the 75% of sediments or sedimentary rocks covering the earth including all of Lesotho, almost the whole of Free State, and large parts of the Eastern Cape, Northern Cape, Mpumalanga and KwaZulu-Natal Provinces of South Africa. Karoo supergroup outcrops are also found in Namibia, Eswatini, Zambia, Zimbabwe and Malawi, as well as on other continents that were part of Gondwana. The basins in which it was deposited formed during the formation and breakup of Pangea. The type area of the Karoo Supergroup is the Great Karoo in South Africa, where the most extensive outcrops of the sequence are exposed. Its strata, which consist mostly of shales and sandstones, record an almost continuous sequence of marine glacial to terrestrial deposition from the Late Carboniferous to the Early Jurassic. These accumulated in a retroarc foreland basin called the "main Karoo" Basin. This basin was formed by the subduction and orogenesis along the southern border of what eventually became Southern Africa, in southern Gondwana. Its sediments attain a maximum cumulative thickness of 12 km, with the overlying basaltic lavas (the Drakensberg Group) at least 1.4 km thick.