Baba Diamond Fields
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Baba Diamond Fields
The Baba Diamond Fields is an area of widespread small-scale diamond mines located at the south-western district of Tsholotsho, Matabeleland North province in Zimbabwe, near the border neighbouring Botswana. It lies about 98 km north-west of the city of Bulawayo and has Kalahari sand soils and rock formations which also can be found at the diamond-rich areas of neighbour Botswana. Currently Baba Diamond Fields is owned by Infinity Baba Diamond Group since 2015 and estimated annual diamond production at the mines to be 1 million carats of rough diamonds. Geology of the Deposit The Baba Diamond Fields consists of three kimberlite pipes Pipe(s), PIPE(S) or piping may refer to: Objects * Pipe (fluid conveyance), a hollow cylinder following certain dimension rules ** Piping, the use of pipes in industry * Smoking pipe ** Tobacco pipe * Half-pipe and quarter pipe, semi-circula ..., and are known for recovery of large, high-quality, exceptional Type II diamonds. High quality pin ...
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Baba Diamond Fields
The Baba Diamond Fields is an area of widespread small-scale diamond mines located at the south-western district of Tsholotsho, Matabeleland North province in Zimbabwe, near the border neighbouring Botswana. It lies about 98 km north-west of the city of Bulawayo and has Kalahari sand soils and rock formations which also can be found at the diamond-rich areas of neighbour Botswana. Currently Baba Diamond Fields is owned by Infinity Baba Diamond Group since 2015 and estimated annual diamond production at the mines to be 1 million carats of rough diamonds. Geology of the Deposit The Baba Diamond Fields consists of three kimberlite pipes Pipe(s), PIPE(S) or piping may refer to: Objects * Pipe (fluid conveyance), a hollow cylinder following certain dimension rules ** Piping, the use of pipes in industry * Smoking pipe ** Tobacco pipe * Half-pipe and quarter pipe, semi-circula ..., and are known for recovery of large, high-quality, exceptional Type II diamonds. High quality pin ...
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Tsholotsho
Tsholotsho is a district in Matabeleland North province in Zimbabwe. Its administrative centre is at Tsholotsho business centre which is located about 98 km north-west of Bulawayo. Districts around Tsholotsho include Lupane, Hwange, Umguza, and Bulilima. The Manzamnyama River separates Tsholotsho from Bulilima District, whilst the Gwayi River separates it from Umguza and Lupane districts, and the Hwange National Park separates it from Hwange District. History The area was a favourite of the elephant herds and had attracted early ivory hunters. The area was occupied by the Bakalanga and San people before Mzilikazi and his Ndebele people arrived here. The name "Tsholotsho" (old spelling "Tjolotjo") being derived from the San word "Tsoro o tso" meaning the head of an elephant. Among the pre-Mzilikazi chiefs of the area were Tategulu, Makulukusa, and Madlangombe. It was part of the Kingdom of Butua and the king or ''mambo madlimbewu'' or ''dlimbewu'' was based at Khami at ...
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Matabeleland North
Matabeleland North is a province in western Zimbabwe. With a population of 749,017 as of the 2012 census, it is the country's second-least populous province, after Matabeleland South, and is the country's least densely populated province. Matabeleland North was established in 1974, when the original Matabeleland Province was divided into two provinces, the other being Matabeleland South. In 1997, the province lost territory when the city of Bulawayo became its own province. Matabeleland North is divided into seven districts. Its capital is Lupane, and Victoria Falls and Hwange are its largest towns. The name "Matabeleland" is derived from the Matabele or Ndebele people, the province's largest ethnic group. Matabeleland North is bordered by Matabeleland South and Bulawayo to the south, Midlands to the east, Mashonaland West to the northeast, Botswana to the west, and Zambia to the north, which is separated from Zimbabwe by the Zambezi river. It has an area of , equal to 19.2% ...
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Zimbabwe
Zimbabwe (), officially the Republic of Zimbabwe, is a landlocked country located in Southeast Africa, between the Zambezi and Limpopo Rivers, bordered by South Africa to the south, Botswana to the south-west, Zambia to the north, and Mozambique to the east. The capital and largest city is Harare. The second largest city is Bulawayo. A country of roughly 15 million people, Zimbabwe has 16 official languages, with English, Shona, and Ndebele the most common. Beginning in the 9th century, during its late Iron Age, the Bantu people (who would become the ethnic Shona) built the city-state of Great Zimbabwe which became one of the major African trade centres by the 11th century, controlling the gold, ivory and copper trades with the Swahili coast, which were connected to Arab and Indian states. By the mid 15th century, the city-state had been abandoned. From there, the Kingdom of Zimbabwe was established, followed by the Rozvi and Mutapa empires. The British Sout ...
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Bulawayo
Bulawayo (, ; Ndebele: ''Bulawayo'') is the second largest city in Zimbabwe, and the largest city in the country's Matabeleland region. The city's population is disputed; the 2022 census listed it at 665,940, while the Bulawayo City Council claimed it to be about 1.2 million. Bulawayo covers an area of about in the western part of the country, along the Matsheumhlope River. Along with the capital Harare, Bulawayo is one of two cities in Zimbabwe that is also a province. Bulawayo was founded by a group led by Gundwane Ndiweni around 1840 as the kraal of Mzilikazi, the Ndebele king and was known as Gibixhegu. His son, Lobengula, succeeded him in the 1860s, and changed the name to kobulawayo and ruled from Bulawayo until 1893, when the settlement was captured by British South Africa Company soldiers during the First Matabele War. That year, the first white settlers arrived and rebuilt the town. The town was besieged by Ndebele warriors during the Second Matabele War. Bulaway ...
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Botswana
Botswana (, ), officially the Republic of Botswana ( tn, Lefatshe la Botswana, label= Setswana, ), is a landlocked country in Southern Africa. Botswana is topographically flat, with approximately 70 percent of its territory being the Kalahari Desert. It is bordered by South Africa to the south and southeast, Namibia to the west and north, and Zimbabwe to the northeast. It is connected to Zambia across the short Zambezi River border by the Kazungula Bridge. A country of slightly over 2.3 million people, Botswana is one of the most sparsely populated countries in the world. About 11.6 percent of the population lives in the capital and largest city, Gaborone. Formerly one of the world's poorest countries—with a GDP per capita of about US$70 per year in the late 1960s—it has since transformed itself into an upper-middle-income country, with one of the world's fastest-growing economies. Modern-day humans first inhabited the country over 200,000 years ago. The Tswana ethn ...
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Kimberlite
Kimberlite is an igneous rock and a rare variant of peridotite. It is most commonly known to be the main host matrix for diamonds. It is named after the town of Kimberley in South Africa, where the discovery of an diamond called the Star of South Africa in 1869 spawned a diamond rush and the digging of the open-pit mine called the Big Hole. Previously, the term kimberlite has been applied to olivine lamproites as Kimberlite II, however this has been in error. Kimberlite occurs in the Earth's crust in vertical structures known as kimberlite pipes, as well as igneous dykes. Kimberlite also occurs as horizontal sills. Kimberlite pipes are the most important source of mined diamonds today. The consensus on kimberlites is that they are formed deep within the mantle. Formation occurs at depths between , potentially from anomalously enriched exotic mantle compositions, and they are erupted rapidly and violently, often with considerable carbon dioxide and other volatile component ...
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Volcanic Pipe
Volcanic pipes or volcanic conduits are subterranean geological structures formed by the violent, supersonic eruption of deep-origin volcanoes. They are considered to be a type of ''diatreme''. Volcanic pipes are composed of a deep, narrow cone of solidified magma (described as "carrot-shaped"), and are usually largely composed of one of two characteristic rock types — kimberlite or lamproite. These rocks reflect the composition of the volcanoes' deep magma sources, where the Earth is rich in magnesium. Volcanic pipes are relatively rare. They are well known as the primary source of diamonds, and are mined for this purpose. Formation Volcanic pipes form as the result of violent eruptions of deep-origin volcanoes. These volcanoes originate at least three times as deep as most other volcanoes, and the resulting magma that is pushed toward the surface is high in magnesium and volatile compounds such as water and carbon dioxide. As the body of magma rises toward the surface, the ...
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