Molepolole is a large village in Kweneng District , Botswana .
31-682: The people who reside in Molepolole are called Bakwena , who are one of the eight major tribes in Botswana. The Bakwena Kgosi (Chief), Sebele I was among the three chiefs who went to England to seek protection from the British in the colonial era. Molepolole serves as the capital of the Bakwena . It was named after the Molepolole river. It is one of the largest traditional villages in Africa with
62-572: A population of over 73,102 people as of 2011. It lies 50 kilometres west of the national capital Gaborone and acts as gateway for exploring the Kalahari Desert . It has a large traditional kgotla and the Scottish Livingstone Hospital , is found in Molepolole. Ntsweng was the capital of Bakwena before they moved to Molepolole. Ntsweng is a historic site located a few kilometers southeast of Molepolole. The area
93-531: Is a stub . You can help Misplaced Pages by expanding it . Kalahari The Kalahari Desert is a large semi-arid sandy savanna in Southern Africa extending for 900,000 square kilometres (350,000 sq mi), covering much of Botswana , as well as parts of Namibia and South Africa . It is not to be confused with the Angolan, Namibian, and South African Namib coastal desert, whose name
124-611: Is a Sotho/Tswana/Sepedi word meaning " crocodile ", the crocodile is also their totem ( seboko ). Earliest ancestor of the Kwena clan, Kwena, was a grandson of Masilo I, the King of Bahurutse clan around 1360 CE. Kwena and his followers settled at Tebang, now called Heidelberg . Around 1500 CE, Bakwena started spreading in the region, from the Lekwa River to Kalahari (Botswana) until settling at Ntsoanatsatsi (mythical origin land of
155-470: Is also Nampol Technical College which is a privately run tertiary institution. Molepolole is the home to many species of plants that thrive in the semi-arid environment. Bakwena The Bakwena or Bakoena ("those who venerate the crocodile ") are a large Sotho-Tswana clan in Southern Africa of the southern Bantu group . They can be found in different parts of southern Africa such as Lesotho , Botswana , South Africa and Eswatini . "Kwena"
186-650: Is home to the lion ( Panthera leo ), cheetah ( Acinonyx jubatus ), African leopard ( Panthera pardus ), spotted hyena ( Crocuta crocuta ), brown hyena ( Parahyaena brunnea ), and African wild dog ( Lycaon pictus pictus ). Birds of prey include the secretarybird ( Sagittarius serpentarius ), martial eagle ( Polemaetus bellicosus ) and other eagles, the giant eagle owl ( Bubo lacteus ) and other owls, falcons , goshawks , kestrels , and kites . Other animals include wildebeest , springbok , gemsbok and other antelopes , Cape porcupines ( Hystrix africaeaustralis ), and ostriches ( Struthio camelus ). Some of
217-514: Is of Khoekhoegowab origin and means "vast place". Kalahari is derived from the Tswana word Kgala , meaning "the great thirst", or Kgalagadi , meaning "a waterless place"; the Kalahari has vast areas covered by red sand without any permanent surface water. The Kalahari Desert was not always a dry desert. The fossil flora and fauna from Gcwihaba Cave in Botswana indicates that the region
248-697: Is situated in the Kalahari Basin . In 1996, De Beers evaluated the potential of diamond mining at Gope. In 1997, the eviction of the San and Bakgalagadi tribes in the Central Kalahari Game Reserve from their land began. In 2006, a Botswana High Court ruled in favor of the San and Bakgalagadi tribes in the reserve, finding their eviction unlawful. The Government of Botswana granted a permit to De Beers' Gem Diamonds/Gope Exploration Company (Pty) Ltd. to conduct mining activities within
279-1099: Is the home to a number of educational institutions that offers education from primary school to tertiary level. The tertiary institutions in Molepolole include Molepolole College of Education which offers diploma in education and Institute of Health Sciences which offers diploma in Nursing. Kgari Sechele Senior Secondary School is the only government-run senior secondary school in Molepolole and it offers Botswana General Certificate of Secondary Education (BGCSE). There are 8 government-run junior secondary schools in Molepolole namely: There are 17 government run primary schools in Molepolole namely; Private schools include Bluebows English medium school which offers pre-school, primary school and secondary school and Kweneng International Secondary School. The other 4 privately owned schools are Shepherd English Medium, Al-haq English Medium, Kgomotso English Medium Primary School (now Regent Hill) and Emmanuel Adventist Academy (formerly Meadows English Medium) which offer pre-primary and primary education only. There
310-568: Is the largest documented non-subglacial underground lake. Such reserves may partly be the residues of ancient lakes; the Kalahari Desert was once a much wetter place. The ancient Lake Makgadikgadi dominated the area, covering the Makgadikgadi Pan and surrounding areas, but it drained or dried out some 10,000 years ago. It may have once covered as much as 120,000 square kilometres (46,000 sq mi). In ancient times, there
341-481: The "central cattle pattern", a conceptual model for the organization of settlements among southern Bantu, where the central placement of the kraal reflects the central role of cattle in the culture and ideology of the people. The Botswana Prison Service (BPS) operates the Molepolole Prison. Molepolole Police Station Scottish Livingston Hospital Mafenyatlala mall Molepolole Stadium Molepolole
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#1732772769773372-763: The Kalahari "desert" is dry enough to qualify as a desert in the sense of having low precipitation , it is not strictly speaking a desert because it has too dense a ground cover. The main region that lacks ground cover is in the southwest Kalahari (southeast of Namibia, northwest of South Africa, and southwest of Botswana) in the south of the Kgalagadi Transfrontier Park . For instance, in the ZF Mgcawu District Municipality of South Africa, total vegetation cover may be as low as 30.72% on non-protected (from cattle grazing) farmlands south of Twee Rivieren Rest Camp and 37.74% in
403-589: The Kalahari "desert", but in the Kalahari basin, halophytic vegetation to the north is adapted to pans, lakes that are completely dry during the dry season, and maybe for years during droughts, such as in Etosha ( Etosha Pan halophytics AT0902) and Makgadikgadi ( Zambezian halophytics AT0908). A totally different vegetation is adapted to the perennial fresh water of the Okavango Delta , an ecoregion termed Zambezian flooded grasslands AT0907. The Kalahari
434-731: The Sotho-Tswana people) with the Bafokeng around 1580 CE. and it continues to the royal line of Lesotho. Kgabo II led a small group of Bakwena and crossed the Madikwe River and founded a tribe on the lands of the Bakgatla tribe (whose totem was the blue monkey) which they drove away, modern day Botswana. As the result of a split, several tribes like the Ngwato and Ngwaketse . This article about an ethnic group in Africa
465-758: The areas within the Kalahari are seasonal wetlands , such as the Makgadikgadi Pans of Botswana . This area, for example, supports numerous halophilic species, and in the rainy season, tens of thousands of flamingos visit these pans. The following protected areas were established in the Kalahari: The San people have lived in the Kalahari for 20,000 years as hunter-gatherers . They hunt wild game with bows and poisoned arrows and gather edible plants, such as berries, melons and nuts, as well as insects. The San get most of their water requirements from plant roots and desert melons found on or under
496-501: The central northern reaches of the Kalahari and provide standing pools of water during the rainy season. A semi-desert, with huge tracts of excellent grazing after good rains, the Kalahari supports more animals and plants than a true desert, such as the Namib Desert to the west. There is little rainfall, and the summer temperature is very high. The driest areas usually receive 110–200 mm (4.3–7.9 in) of rain per year, and
527-603: The climate is drier, it becomes a true semi-desert with ground not entirely covered by vegetation: "open" as opposed to "closed" vegetation. Examples include the north of the ZF Mgcawu District Municipality , itself in the north of South Africa, and the Keetmanshoop Rural in the southeast of Namibia. In the north and east, dry forests cover an area of over 300,000 km in which Rhodesian teak and several species of acacia are prominent. These regions are termed Kalahari Acacia-Baikiaea woodlands AT0709. Outside
558-429: The desert floor. They often store water in the blown-out shells of ostrich eggs. The San live in huts built from local materials—the frame is made of branches, and the roof is thatched with long grass. Most of their hunting and gathering techniques replicate pre-historic tribes. Bantu -speaking Tswana , Kgalagadi , and Herero and a small number of European settlers also live in the Kalahari desert. The city of Windhoek
589-589: The driest and sunniest parts of the Kalahari, over 4,000 hours of sunshine are recorded annually on average. In the Kalahari, there are three main mechanisms of atmospheric circulation, dominated by the Kalahari High anticyclone in winter, and by the Kalahari Heat Low in summer: There are huge subterranean water reserves beneath parts of the Kalahari; the Dragon's Breath Cave , for example,
620-456: The latter, the area of the Kalahari has expanded to include parts of western Zimbabwe, Zambia, and Angola. Due to its low aridity, the Kalahari supports a variety of flora. The native flora includes acacia trees and many other herbs and grasses. The kiwano fruit, also known as the horned melon, melano, African horned cucumber, jelly melon, or hedged gourd, is endemic to a region in the Kalahari Desert (specific region unknown). Even where
651-486: The protected (from cattle grazing) South African side of the Kgalagadi Transfrontier Park: these southernmost Kalahari xeric savanna areas are truly semi-deserts. However, in all the remaining Kalahari, except on salt pans during the dry season, the vegetation cover can be denser, up to almost 100%, in some limited areas. In an area of about 600,000 km in the south and west of the Kalahari,
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#1732772769773682-425: The ruins of what used to be Sebele II's office which is at present referred to as Mmakgosi's house. The ruins of that building are situated next to an area which used to be the royal kraal at Ntsweng but is now the royal cemetery. Several clusters of ruins seem to represent different wards. Analyses of the settlement layout and soil samples suggest cattle were often kept in the center of each ward. This seems to follow
713-518: The vegetation is mainly xeric savanna . This area is the ecoregion identified by World Wide Fund for Nature as Kalahari xeric savanna AT1309. Typical savanna grasses include Schmidtia , Stipagrostis , Aristida , and Eragrostis ; these are interspersed with trees such as camelthorn ( Acacia erioloba ), grey camelthorn ( Acacia haematoxylon ), shepherd's tree ( Boscia albitrunca ), blackthorn ( Acacia mellifera ), and silver cluster-leaf ( Terminalia sericea ). In certain areas where
744-421: The vegetation is predominantly xeric savanna or even a semi-desert, the climate is "Kalaharian" semi-arid . The Kalaharian climate is subtropical (average annual temperature greater than or equal to 18 °C, at peaks reaching 40 °C and above, with mean monthly temperature of the coldest month strictly below 18 °C), and is semi-arid with the dry season from April to September, the coldest six months of
775-605: The warmer Sahelian regions. For the same reason, summer temperatures certainly can be very hot, but not in comparison to regions of low altitude in the Sahel or Sahara, where some stations record average temperatures of the warmest month around 38 °C, whereas the average temperature of the warmest month in any region in the Kalahari never exceeds 29 °C, though daily temperatures occasionally reach up to close to 45 °C (113 °F) (44.8 °C at Twee Rivieren Rest Camp in 2012). The dry season lasts eight months or more, and
806-439: The wet season typically from less than one month to four months, depending on location. The southwestern Kalahari is the driest area, particularly a small region toward the west-southwest of Tsaraxaibis (Southeast of Namibia). The average annual rainfall ranges from around 110 mm (close to aridity) to more than 500 mm in some north and east areas. During summertime in all regions, rainfall may go with heavy thunderstorms. In
837-419: The wettest just a little over 500 mm (20 in). The surrounding Kalahari Basin covers over 2,500,000 km (970,000 sq mi) extending farther into Botswana, Namibia, and South Africa, encroaching into parts of Angola , Zambia and Zimbabwe . The climate is sub-humid rather than semi-arid in the north and east, where the dry forests, savannahs, and salt lakes prevail. South and west, where
868-539: The year. It is the southern tropical equivalent of the Sahelian climate with the wet season during summer. The altitude has been adduced as the explanation why the Kalaharian climate is not tropical; its altitude ranges from 600 to 1600 meters (and generally from 800 to 1200 meters), resulting in a cooler climate than that of the Sahel or Sahara . For example, winter frost is common from June to August, rarely seen in
899-418: Was first occupied by Bakwena, led by Sechele I (ruled 1829–92), in 1864. It was abandoned in 1937 when Bakwena were forced to move to Molepolole by Kgari II, assisted by the colonial administrators. Ntsweng today consists of a large area covered with traces of occupation. Most notable are the patterns of stones laid on their edges that form house foundations which are still visible on the surface. There are also
930-624: Was much wetter and cooler at least from 30 to 11 thousand Before Present , especially after 17,500 BP. Drainage of the desert is by dry black valleys, seasonally inundated pans, and the large salt pans of the Makgadikgadi Pan in Botswana and Etosha Pan in Namibia. The only permanent river, the Okavango , flows into a delta in the northwest, forming marshes that are rich in wildlife. Ancient dry riverbeds—called omuramba —traverse
961-472: Was sufficient moisture for farming, with dikes and dams collecting the water. These are now filled with sediment, breached, or no longer in use, though they can be readily seen via Google Earth. The Kalahari has had a complex climatic history over the past million or so years, in line with major global changes. Changes in the last 250,000 years have been reconstructed from various data sources, providing evidence of former extensive lakes and drier periods. During