KwaZulu-Natal Province in the context of "Olea"

Shaka kaSenzangakhona (c. 1787–24 September 1828), also known as Shaka (the) Zulu (Zulu pronunciation: [ˈʃaːɠa]) and Sigidi kaSenzangakhona, was the king of the Zulu Kingdom from 1816 to 1828. One of the most influential monarchs of the Zulu, he ordered wide-reaching reforms that reorganized the military into a formidable force.

King Shaka was born in the lunar month of uNtulikazi (July) in 1787, in Mthonjaneni, KwaZulu-Natal Province, South Africa. The son of the Zulu King Senzangakhona kaJama, he was spurned as an illegitimate son. Shaka spent part of his childhood in his mother's settlements, where he was initiated into an ibutho lempi (fighting unit/regiment), serving as a warrior under Inkosi Dingiswayo.

The Chewa are a Bantu ethnic group primarily found in Malawi and Zambia, with few populations in Zimbabwe and Mozambique. The Chewa are closely related to people in surrounding regions such as the Tumbuka. As with the Nsenga and Tumbuka, a small part of Chewa territory came under the influence of the Ngoni, who were of Zulu or Natal/Transvaal origin. An alternative name, often used interchangeably with Chewa, is Nyanja. Their language is called Chichewa. The Chewa are mainly known for their masks and their secret societies, called Nyau.

The Chewa (Mang'anja) are a remnant of the Maravi people.

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.