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Beaufort-Wes
Beaufort West (Afrikaans: ''Beaufort-Wes''; Xhosa: ''eBhofolo'') is a town in the Western Cape province in South Africa. It is the largest town in the arid Great Karoo region, and is known as the "Capital of the Karoo". It forms part of the Beaufort West Local Municipality, with 34,085 inhabitants in 2011. It is the centre of an agricultural district based mainly on sheep farming, and is a significant town and logistical support hub on the N1 national road. Next door to Beaufort West is the Karoo National Park. Important Permian era fossils have been found in the area to the west of the town. Initially found by David Baird, son of the local magistrate in 1827. The old Town Hall and the Dutch Reformed Church have been declared national monuments. History Beaufort West was the first town to be established in the central Karoo. The town was founded in 1818 and initially named ''Beaufort'' after Henry Somerset, 5th Duke of Beaufort, who was the father of Lord Charles Henry Somerset, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Beaufort West Local Municipality
Beaufort West Local Municipality ( af, Beaufort-Wes Plaaslike Munisipaliteit) is a municipality located in Western Cape Province, South Africa. the population is 49,586. Its municipality code is WC053. Geography The municipality covers an area of , making it the largest local municipality in the Western Cape and the sixth-largest in South Africa. It is located in the furthest northeastern part of the province in the Great Karoo. It abuts on the Karoo Hoogland Municipality to the northwest, the Ubuntu Municipality to the north, the Dr Beyers Naudé Municipality to the southeast, the Prince Albert Municipality to the south and the Laingsburg Municipality to the southwest. According to the 2011 census the municipality has a population of 49,586 people in 13,089 households. Of this population, 73.5% describe themselves as "Coloured", 16.3% as "African", and 9.2% as "White". The first language of 84.3% of the population is Afrikaans, while 10.7% speak Xhosa and 2.5% speak Engli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Diictodontia
The Diictodontia were a group of herbivorous Dicynodonts from the Permian and Triassic of South Africa. The clade was named a sub group of the group Dicynodontia by Robert L. Carroll in 1988. Image:Diictodon-A72-03.jpg, A model of the genus ''Diictodon'' Image:Myosaurus.jpg, ''Myosaurus ''Myosaurus'' is an extinct genus of dicynodont found primarily in Antarctica and South Africa. History The family Myosauridae is known only from fossilized skull specimens. The family is distinguished from other families in the infraorder Dic ...'', an Emydopid Image:Diictodon.jpg, A ''Diictodon'' fossil References {{Taxonbar, from=Q5276469 Dicynodonts Guadalupian first appearances Lopingian extinctions ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
English Language
English is a West Germanic language of the Indo-European language family, with its earliest forms spoken by the inhabitants of early medieval England. It is named after the Angles, one of the ancient Germanic peoples that migrated to the island of Great Britain. Existing on a dialect continuum with Scots, and then closest related to the Low Saxon and Frisian languages, English is genealogically West Germanic. However, its vocabulary is also distinctively influenced by dialects of France (about 29% of Modern English words) and Latin (also about 29%), plus some grammar and a small amount of core vocabulary influenced by Old Norse (a North Germanic language). Speakers of English are called Anglophones. The earliest forms of English, collectively known as Old English, evolved from a group of West Germanic (Ingvaeonic) dialects brought to Great Britain by Anglo-Saxon settlers in the 5th century and further mutated by Norse-speaking Viking settlers starting in the 8th and 9th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fort Beaufort
Fort Beaufort (Xhosa: iBhofolo) is a town in the Amatole District of South Africa's Eastern Cape Province, and had a population of 25,668 in 2011. The town was established in 1837 and became a municipality in 1883. The town lies at the confluence of the Kat River and Brak River between the Keiskamma and Great Fish Rivers. Fort Beaufort serves as a mini-'dormitory' for academic staff and students of Fort Hare University, based in the nearby town of Alice, and is also close to Sulphur Springs. It is also the birthplace of South African politician and anti-apartheid activist who is also the first Premier of the Eastern Cape Raymond Mhlaba and his former first wife Joyce Meke. History The roots of Fort Beaufort is a mission station that the Reverend Joseph Williams of the London Missionary Society established in 1816. In 1822, Colonel Maurice Scott of the Royal Warwickshire Regiment constructed a blockhouse about three miles from the mission station as a military frontier post and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cape Colony
The Cape Colony ( nl, Kaapkolonie), also known as the Cape of Good Hope, was a British Empire, British colony in present-day South Africa named after the Cape of Good Hope, which existed from 1795 to 1802, and again from 1806 to 1910, when it united with three other colonies to form the Union of South Africa. The British colony was preceded by an earlier corporate colony that became an Dutch Cape Colony, original Dutch colony of the same name, which was established in 1652 by the Dutch East India Company, Dutch East India Company (VOC). The Cape was under VOC rule from 1652 to 1795 and under rule of the Napoleonic Batavian Republic, Batavia Republic from 1803 to 1806. The VOC lost the colony to Kingdom of Great Britain, Great Britain following the 1795 Invasion of the Cape Colony, Battle of Muizenberg, but it was acceded to the Batavian Republic, Batavia Republic following the 1802 Treaty of Amiens. It was re-occupied by the British following the Battle of Blaauwberg in 1806 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lord Charles Henry Somerset
Lord Charles Henry Somerset PC (12 December 1767 – 18 February 1831), born in Badminton, England, was a British soldier, politician and colonial administrator.Charles Mosley, editor. Burke's Peerage and Baronetage, 106th edition, 2 volumes (Crans, Switzerland: Burke's Peerage (Genealogical Books) Ltd, 1999), volume 1, page 221 – 223. He was governor of the Cape Colony, South Africa, from 1814 to 1826. Background Somerset was the second son of Henry Somerset, 5th Duke of Beaufort, and Elizabeth, daughter of Admiral the Hon. Edward Boscawen. He was the brother of Henry Somerset, 6th Duke of Beaufort, General Lord Robert Somerset, Lord Arthur Somerset and Field Marshal FitzRoy Somerset, 1st Baron Raglan. Political career Somerset sat as member of parliament for Scarborough between 1796 and 1802 and for Monmouth Boroughs between 1802 and 1813. He served as Comptroller of the Household between 1797 and 1804 and as Joint Paymaster of the Forces between 1804 and 1806 and 1 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Henry Somerset, 5th Duke Of Beaufort
Henry Somerset, 5th Duke of Beaufort (16 October 1744 – 11 October 1803) was an English courtier and politician. He was the only son of Charles Noel Somerset, 4th Duke of Beaufort and Elizabeth Somerset, Duchess of Beaufort. Styled Marquess of Worcester from 1746, at his father's death on 28 October 1756, he succeeded him as 5th Duke of Beaufort, 7th Marquess of Worcester, 11th Earl of Worcester, and 13th Baron Herbert.G. E. Cokayne; with Vicary Gibbs, H.A. Doubleday, Geoffrey H. White, Duncan Warrand and Lord Howard de Walden, editors. The Complete Peerage of England, Scotland, Ireland, Great Britain and the United Kingdom, Extant, Extinct or Dormant, new ed., 13 volumes in 14 (1910-1959; reprint in 6 volumes, Gloucester, U.K.: Alan Sutton Publishing, 2000), volume II, page 55. Life On 18 October 1760, he began his studies at Oriel College, Oxford, graduating on 7 July 1763 with a Doctor of Civil Laws (DCL) degree. He held the office of Grand Master of the Premier Gran ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fossils
A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved in amber, hair, petrified wood and DNA remnants. The totality of fossils is known as the ''fossil record''. Paleontology is the study of fossils: their age, method of formation, and evolutionary significance. Specimens are usually considered to be fossils if they are over 10,000 years old. The oldest fossils are around 3.48 billion years old to 4.1 billion years old. Early edition, published online before print. The observation in the 19th century that certain fossils were associated with certain rock strata led to the recognition of a geological timescale and the relative ages of different fossils. The development of radiometric dating techniques in the early 20th century allowed scientists to quantitatively measure the absolute ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Permian
The Permian ( ) is a geologic period and stratigraphic system which spans 47 million years from the end of the Carboniferous Period million years ago (Mya), to the beginning of the Triassic Period 251.9 Mya. It is the last period of the Paleozoic Era; the following Triassic Period belongs to the Mesozoic Era. The concept of the Permian was introduced in 1841 by geologist Sir Roderick Murchison, who named it after the region of Perm in Russia. The Permian witnessed the diversification of the two groups of amniotes, the synapsids and the sauropsids ( reptiles). The world at the time was dominated by the supercontinent Pangaea, which had formed due to the collision of Euramerica and Gondwana during the Carboniferous. Pangaea was surrounded by the superocean Panthalassa. The Carboniferous rainforest collapse left behind vast regions of desert within the continental interior. Amniotes, which could better cope with these drier conditions, rose to dominance in place of their am ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karoo National Park
The Karoo ( ; from the Afrikaans borrowing of the South Khoekhoe Khoe languages, !Orakobab or Khoemana word ''ǃ’Aukarob'' "Hardveld") is a semi-desert natural region of South Africa. No exact definition of what constitutes the Karoo is available, so its extent is also not precisely defined. The Karoo is partly defined by its topography, Karoo Supergroup, geology and climate, and above all, its low rainfall, arid air, cloudless skies, and extremes of heat and cold.Potgieter, D.J. & du Plessis, T.C. (1972) ''Standard Encyclopaedia of Southern Africa''. Vol. 6. pp. 306–307. Nasou, Cape Town.''Reader’s Digest Illustrated Guide to Southern Africa''. (5th Ed. 1993). pp. 78–89. Reader’s Digest Association of South Africa Pty. Ltd., Cape Town. The Karoo also hosted a well-preserved ecosystem hundreds of million years ago which is now represented by many fossils. The ǃ’Aukarob formed an almost impenetrable barrier to the interior from Cape Town, and the early adventurers, ex ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
N1 (South Africa)
The N1 is a national route in South Africa that runs from Cape Town through Bloemfontein, Johannesburg, Pretoria and Polokwane to Beit Bridge on the border with Zimbabwe. It forms the first section of the famed Cape to Cairo Road. Prior to 1970, the N1 designation was applied to the route from Beit Bridge to Colesberg and then along the current N9 to George. The section from Cape Town to Colesberg was designated the N9.http://www.theheritageportal.co.za/sites/default/files/styles/adaptive/public/Department%20of%20Transport%20Map%20South%20Africa%201959.jpg?itok=TncXhikX Route Western Cape The N1 begins in central Cape Town at the northern end of Buitengracht Street (M62), outside the entrance to the Victoria & Alfred Waterfront. The first section of the N1 is shared with the beginning of the N2; it is a four-lane elevated freeway that runs along a strip of land between the city centre and the Port of Cape Town. On the eastern edge of the city centre the two roads sp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karoo
The Karoo ( ; from the Afrikaans borrowing of the South Khoekhoe !Orakobab or Khoemana word ''ǃ’Aukarob'' "Hardveld") is a semi-desert natural region of South Africa. No exact definition of what constitutes the Karoo is available, so its extent is also not precisely defined. The Karoo is partly defined by its topography, geology and climate, and above all, its low rainfall, arid air, cloudless skies, and extremes of heat and cold.Potgieter, D.J. & du Plessis, T.C. (1972) ''Standard Encyclopaedia of Southern Africa''. Vol. 6. pp. 306–307. Nasou, Cape Town.''Reader’s Digest Illustrated Guide to Southern Africa''. (5th Ed. 1993). pp. 78–89. Reader’s Digest Association of South Africa Pty. Ltd., Cape Town. The Karoo also hosted a well-preserved ecosystem hundreds of million years ago which is now represented by many fossils. The ǃ’Aukarob formed an almost impenetrable barrier to the interior from Cape Town, and the early adventurers, explorers, hunters, and travelers o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
