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 from 1000 AD. Construction on the city began in the 11th century and continued until it was abandoned in the 16th or 17th 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). The Zimbabwe state covered 50,000 km². It is recognised as a World Heritage Site by UNESCO.
Khami is a ruined city located 22 kilometres (14 mi) west of Bulawayo, in Zimbabwe. It was once the capital of the Kingdom of Butua of the Torwa dynasty. It is now a national monument and became a UNESCO World Heritage Site in 1986.
The Kingdom of Mapungubwe was an ancient state located at the confluence of the Shashe and Limpopo rivers in South Africa, south of Great Zimbabwe. The capital's population was 5000 by 1250, and the state likely covered 30,000 km².
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.
Ing'ombe Ilede is an archaeological site located on a hill near the confluence of the Zambezi and Lusitu rivers, near the town of Siavonga, in Zambia. Ing'ombe Ilede, meaning "a sleeping cow", received its name from a local baobab tree that is partially lying on the ground and resembles a sleeping cow from a distance. The site is thought to have been a small commercial state around the 16th century whose chief item of trade was salt. Ing'ombe Ilede received various goods from the hinterland of south-central Africa, such as, copper, slaves, gold and ivory. These items were exchanged with glass beads, cloth, cowrie shells from the Indian Ocean trade. The status of Ing'ombe Ilede as a trading center that connected different places in south-central Africa has made it a very important archaeological site in the region.
The pre-colonial history of Zimbabwe lasted until the British government granted colonial status to Southern Rhodesia in 1923.
Zimbabwean art includes decorative esthetics applied to many aspects of life, including art objects as such, utilitarian objects, objects used in religion, warfare, in propaganda, and in many other spheres. Within this broad arena, Zimbabwe has several identifiable categories of art. It is a hallmark of African cultures in general that art touches many aspects of life, and most tribes have a vigorous and often recognisable canon of styles and a great range of art-worked objects. These can include masks, drums, textile decoration, beadwork, carving, sculpture, ceramic in various forms, housing and the person themselves. Decoration of the body in permanent ways such as scarification or tattoo or impermanently as in painting the body for a ceremony is a common feature of African cultures.
Chibuene is a Mozambican archaeological site, located five kilometres south of the coastal city of Vilanculos South Beach. The site was occupied during two distinct phases. The earlier phase of occupation dates to the late first millennium AD. The second phase dates from around 1450 and is contemporaneous with the Great Zimbabwe civilization in the African interior. During both phases of its development Chibuene was a trading settlement. Trade goods obtained from the site include glass beads, painted blue and white ceramics, and glass bottle fragments. The later phase of settlement has yielded remains of medieval structures as well as evidence of metallurgy. Crucibles have been found that were presumably used to melt gold obtained from trade with the Great Zimbabwe civilization. There is evidence that Chibuene traded extensively with the inland settlement of Manyikeni. Mozambique has jointly inscribed these two properties on their tentative version of the World Heritage List.
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.
Enkapune Ya Muto, also known as Twilight Cave, is a site spanning the late Middle Stone Age to the Late Stone Age on the Mau Escarpment of Kenya. This time span has allowed for further study of the transition from the Middle Stone Age to the Late Stone Age. In particular, the changes in lithic and pottery industries can be tracked over these time periods as well as transitions from a hunter-gatherer lifestyle to a herding lifestyle. Beads made of perforated ostrich egg shells found at the site have been dated to 40,000 years ago. The beads found at the site represent the early human use of personal ornaments. Inferences pertaining to climate and environment changes during the pre-Holocene and Holocene period have been made based from faunal remains based in this site.
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 was Great Zimbabwe, in today's Masvingo, and is the largest stone structure in precolonial Southern Africa. The kingdom came about after the collapse of the Kingdom of Mapungubwe. The Zimbabwe state covered 50,000 km².
Bambandyanalo or K2 is an archaeological site in present-day South Africa, just south 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. 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. It was closely associated with Mapungubwe and was a precursor to the much better known Great Zimbabwe near Masvingo, 125 miles to the northeast.
Thimlich Ohinga is a complex of stone-built ruins in Migori county, Nyanza Kenya, in East Africa. It is the largest one of 138 sites containing 521 stone structures that were built around the Lake Victoria region in Kenya. These sites are highly clustered. The main enclosure of Thimlich Ohinga has walls that are 1–3 m (3.3–9.8 ft) in thickness, and 1–4.2 m (3.3–13.8 ft) in height. The structures were built from undressed blocks, rocks, and stones set in place without mortar. The densely packed stones interlock. The site is believed to date to the 15th century or earlier.
Gogo Falls is an archaeological site near a former and since 1956 dammed waterfall, located in the Lake Victoria Basin in Migori County, western Kenya. This site is important to archaeology as it includes some of the earliest appearances of artifacts and domestic animals in the area. The findings at the site help to reconstruct the later prehistory around Lake Victoria, including a Pastoral Neolithic occupation by Elmenteitan peoples and a later Iron Age occupation. Artifacts found at the site included pottery and iron artifacts. Through these artifacts some of the cultural traditions of the people who lived near Gogo Falls were discovered.
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.
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.
Daima is a mound settlement located in Nigeria, near Lake Chad, and about 5 kilometers away from the Nigerian frontier with Cameroon. It was first excavated in 1965 by British archaeologist Graham Connah. Radiocarbon dating showed the occupations at Daima cover a period beginning early in the first millennium BC, and ending early in the second millennium AD. The Daima sequence then covers some 1800 years. Daima is a perfect example of an archaeological tell site, as Daima’s stratigraphy seems to be divided into three periods or phases which mark separate occupations. These phases are called Daima I, Daima II, and Daima III. Although these occupations differ from each other in multiple ways, they also have some shared aspects with one another. Daima I represents an occupation of a people without metalwork; Daima II is characterized by the first iron-using people of the site; and Daima III represents a rich society with a much more complex material culture.
Mapela Hill is an archaeological site located in southwestern Zimbabwe, 90km northwest of Mapungubwe.
