Bambandyanalo or K2 is an archaeological site in present-day Zimbabwe, just north of the Limpopo River. It flourished from the 11th to 13th centuries, being a predecessor to the Great Zimbabwe culture. The ruins have survived because much of the complex was built in stone. The site contains a large mound, some 180 metres in diameter, and covers an area of about 5 hectares. It is surrounded on three sides by sandstone cliffs (Wood 2005:86). In the 11th century, Bambandyanalo developed its influence over the region and established itself as a hub in the trade connecting the African inland with the Indian Ocean (Hall 1987:83). It was closely associated with Mapungubwe and was a precursor to the much better known Great Zimbabwe near Masvingo, 125 miles to the northeast.
People were buried in areas associated with their life. Women worked copper, while men worked iron. Family heads resolved disputes in their homestead, however external disputes were handled by the court, located near the cattle kraal. The cattle kraal was crucial to a man's life, and the lobola (bride price) was usually paid in cattle. [1] : 16–23
They cultivated sorghum, pearl millet, finger millet, ground beans, and cowpeas. The population expanded, and K2 had a population of 1500 by 1200. Rainmaking was widespread, and the chief sometimes hired strangers, such as the San, who were believed to have special relationships with the spirits of the land due to a longer habitation. Some Zhizo remained at Leokwe, likely subordinate to K2 while specialising in rituals also due to their longer habitation. [2] : 26–29
The large wealth generated by the Indian Ocean trade created unprecedented inequalities, evolving over time from a society based on social ranking to social classes. K2's spatial arrangement became unsuited to this development, and they moved to Mapungubwe. [3] : 30
Great Zimbabwe is a medieval city in the south-eastern hills of the modern country of Zimbabwe, near Lake Mutirikwe and the town of Masvingo. It was the capital of the Kingdom of Zimbabwe from the 13th century, having been settled in the 4th century AD. Construction on the city began in the 11th century and continued until it was abandoned in the 15th century. The edifices were erected by ancestors of the Shona people, currently located in Zimbabwe and nearby countries. The stone city spans an area of 7.22 square kilometres (2.79 sq mi) and could have housed up to 18,000 people at its peak, giving it a population density of approximately 2,500 inhabitants per square kilometre (6,500/sq mi). It is recognised as a World Heritage Site by UNESCO.
Limpopo is the northernmost province of South Africa. It is named after the Limpopo River, which forms the province's western and northern borders. The term Limpopo is derived from Rivombo (Livombo/Lebombo), a group of Tsonga settlers led by Hosi Rivombo who settled in the mountainous vicinity and named the area after their leader. The Lebombo mountains are also named after them. The river has been called the Vhembe by local Venda communities of the area. The capital and largest city in the province is Polokwane, while the provincial legislature is situated in Lebowakgomo.
Southern Africa is the southernmost region of Africa. No definition is agreed upon, but some groupings include the United Nations geoscheme, the intergovernmental Southern African Development Community, and the physical geography definition based on the physical characteristics of the land.
The Kingdom of Mapungubwe was an ancient state in South Africa located at the confluence of the Shashe and Limpopo rivers, south of Great Zimbabwe. The kingdom was the first stage in a development that would culminate in the creation of the Kingdom of Zimbabwe in the 13th century, and with gold trading links to Rhapta and Kilwa Kisiwani on the African east coast. At its height the capital's population was about 5000 people. Although traditionally assumed to have been the first kingdom in Southern Africa, excavations in the same region at Mapela Hill show evidence for sacral kingship nearly 200 years earlier.
The Mapungubwe Collection, held by the University of Pretoria museums in its Old Arts Building, consists of archaeological materials excavated by the former University of Gauteng from the Mapungubwe archaeological site since its discovery in 1933. The collection includes ceramics, metals, trade glass beads, indigenous beads, clay figurines, and artifacts made from bone and ivory, alongside a research collection of potsherds, faunal remains, and other fragmentary materials. In June 2000, the University of Gauteng inaugurated the permanent museum. The collection is maintained on site, serving both educational and tourism purposes.
The Venḓa are a Bantu people native to Southern Africa living mostly near the South African-Zimbabwean border. The Venda language arose from interactions with Sotho-Tswana and Kalanga initiates during the 4th century in Mapungubwe.
The Kaapvaal Craton, along with the Pilbara Craton of Western Australia, are the only remaining areas of pristine 3.6–2.5 Ga crust on Earth. Similarities of rock records from both these cratons, especially of the overlying late Archean sequences, suggest that they were once part of the Vaalbara supercontinent.
The Prehistory of South Africa lasts from the Middle Stone Age until the 17th century. Southern Africa was first reached by Homo sapiens before 130,000 years ago, possibly before 260,000 years ago. The region remained in the Late Stone Age until the first traces of pastoralism were introduced about 2,000 years ago. The Bantu migration reached the area now South Africa around the first decade of the 3rd century, over 1800 years ago. Early Bantu kingdoms were established in the 11th century. First European contact dates to 1488, but European colonization began in the 17th century.
The pre-colonial history of Zimbabwe lasted until the British government granted colonial status to Southern Rhodesia in 1923.
Thomas N. Huffman was Professor Emeritus of archaeology in association with the University of Witwatersrand in Johannesburg, South Africa. He specialised in pre-colonial farming societies in southern Africa. Huffman is most well known for his identification of the Central Cattle Pattern at Mapungubwe, a pre-colonial state in southern Africa. This, in turn he argued as the main influence in the formation of the Zimbabwe Pattern at Great Zimbabwe. Arguably his seminal contribution to the field was A Handbook to the Iron Age: The Archaeology of Pre-Colonial Farming Societies in Southern Africa (2007), which has contributed to the understanding of ceramic style analysis and culture history focusing on these groups.
The Kalanga or BaKalanga are a southern Bantu ethnic group mainly inhabiting Matebeleland in Zimbabwe, northern Botswana, and parts of the Limpopo Province in South Africa.
The Blaauboschkraal stone ruins are a provincial heritage site in the Mpumalanga province of South Africa. Its neighbouring town, Emgwenya, is 10 kilometres away. The site was declared a national monument on 18 April 1975 and is a heritage site recognised by the South African Heritage Resources Agency.
Toutswemogala Hill lies 6.5 km West of the North-South Highway in the Central District of Botswana. It is situated about 50 km north of the village of Palapye. Toutswemogala is an elongated flat-topped hill, geologically called a mesa, rising about 50 meters above the surrounding flat mopane veld. It is an Iron Age settlement, which has been occupied on two occasions. The radio-carbon dates for this settlement range from 7th to late 19th century AD indicating occupation of more than one thousand years. The hill was part of the formation of early states in Southern Africa with cattle keeping as major source of economy. This was supplemented by goats, sheep and foraging as well as hunting of wild animals. The remaining features of Toutswe settlement include house-floors, large heaps of vitrified cow-dung and burials while the outstanding structure is the stone wall. There are large traits of centaurs ciliaris, a type of grass which has come to be associated with cattle-keeping settlements in South, Central Africa.
The Kingdom of Zimbabwe was a medieval Shona kingdom located in modern-day Zimbabwe. Its capital, today's Masvingo, which is commonly called Great Zimbabwe, is the largest stone structure in precolonial Southern Africa. This kingdom came about after the collapse of the Kingdom of Mapungubwe.
Leopard's Kopje is an archaeological site, the type site of the associated region or culture that marked the Middle Iron Age in Zimbabwe. The ceramics from the Leopard's Kopje type site have been classified as part of phase II of the Leopard's Kopje culture. For information on the region of Leopard's Kopje, see the "Associated sites" section of this article.
The following index is provided as an overview of and topical guide to the protected areas of South Africa:
Kweneng’ ruins are the remains of a pre-colonial Tswana capital occupied from the 14th to the 19th century AD in South Africa. The site is located 30km south of the modern-day city of Johannesburg. Settlement at the site likely began around the 1300s and saw its peak in the 14th century. The Kweneng' ruins are similar to those built by other early civilizations found in the southern Africa region during this period, including the Luba–Lunda kingdom, Kingdom of Mutapa, Bokoni, and many others, as these groups share ancestry. Kweneng' was the largest of several sizable settlements inhabited by Tswana speakers prior to European arrival. Several circular stone walled family compounds are spread out over an area 10km long and 2km wide. It is likely that Kweneng' was abandoned in the 1820s during the period of colonial expansion-related civil wars known as the Mfecane or Difaqane, leading to the dispersal of its inhabitants.
The history of Southern Africa has been divided into its prehistory, its ancient history, the major polities flourishing, the colonial period, and the post-colonial period, in which the current nations were formed. Southern Africa is bordered by Central Africa, East Africa, the Atlantic Ocean, the Indian Ocean, and the Sahara Desert. Colonial boundaries are reflected in the modern boundaries between contemporary Southern African states, cutting across ethnic and cultural lines, often dividing single ethnic groups between two or more states.
Bosutswe is an archaeological site at the edge of the Kalahari Desert in Botswana on top of Bosutswe Hill. The site can be dated back to around 700 AD. The location of Bosutswe makes it easy for archaeologists to study as the record of the site is continuous. It is believed that the area was occupied consistently for around 1000 years. It was known for its advanced metalworking which first appeared around 1300 AD, which is known as the Lose Period. The Lose Period is named after the elite class that can be found in the area.
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