45-701: Thornybush Game Reserve is a private game reserve, near Hoedspruit , in the Limpopo province of South Africa . It borders the Kapama Game Reserve and is located close to the Timbavati Game Reserve and the Kruger Park . The Reserve's surface area is approximately 14,000 ha of mainly open savannah . As with many private reserves in South Africa , Thornybush is managed as an eco-tourism destination, thus
90-453: A group of young men, all under 45, established their settlement between the mountain and the Blyde River on a farm they named Jonkmanspruit (meaning "young man river/stream/creek"). Other young men settled on nearby farms named Welverdiend (meaning "well deserved") and Driehoek (meaning "triangle") due to the farm's shape. These original names still exist in the area today and are located around
135-595: Is due to a failed westerly branch of the main rift that caused Antarctica to start drifting away from southern Africa during the breakup of Gondwana about 150 million years ago. The lower Limpopo River and Save River drain into the Indian Ocean through what remains of this relict incipient rift valley, which now forms part of the South African Lowveld . During the past 20 million years, southern Africa has experienced massive uplifting, especially in
180-589: Is formed by slightly younger Beaufort rocks (250 million years old) that also are part of the Karoo Supergroup. The Ecca and Beaufort groups are composed of sedimentary rocks that are less erosion resistant than the other rocks that make up the Drakensberg escarpment. Therefore, this portion of escarpment is not so impressive as the Mpumalanga and Lesotho stretches of the Drakensberg. The Drakensberg that form
225-727: Is home to large herds of grazing fauna and antelopes such as eland (Taurotragus oryx) , reedbuck (Redunca arundinum) , mountain reedbuck (Redunca fulvorufula) , grey rhebok (Pelea capreolus) , and even some oribi (Ourebia ourebi) . Chacma baboons also are present. Endemic species include a large number of chameleons and other reptiles. There is one endemic frog, the forest rain frog ( Breviceps sylvestris ) , and four more species that are found mainly in these mountains; long-toed tree frog ( Leptopelis xenodactylus ) , plaintive rain frog ( Breviceps maculatus ) , rough rain frog ( Breviceps verrucosus ) , and Poynton's caco ( Cacosternum poyntoni ) . The high slopes are hard to reach so
270-774: Is known as 'Klein Drakensberg' by the Afrikaner . From Hoedspruit it extends west to Tzaneen , also in Limpopo Province , where it is known as the Wolkberg Mountains and Iron Crown Mountain. At 2,200 m (7,200 ft) above sea level, the Wolkberg is the highest elevation in Limpopo. The escarpment extends west again and at Mokopane it is known as the Strydpoort Mountains. The Afrikaans name Drakensberge comes from
315-641: Is part of the Transvaal Supergroup, which also forms the Magaliesberg to the north and northwest of Pretoria. These rocks are more than 2000 million years old. South of the 26°S parallel the Drakensberg escarpment is composed of Ecca shales , which belong to the Karoo Supergroup , and they are 300 million years old. The portion of the Drakensberg that forms the KwaZulu-Natal – Free State border
360-614: Is the eastern portion of the Great Escarpment , which encloses the central Southern African plateau. The Great Escarpment reaches its greatest elevation – 2,000 to 3,482 metres (6,562 to 11,424 feet) within the border region of South Africa and Lesotho . The Drakensberg escarpment stretches for more than 1,000 kilometres (600 miles) from the Eastern Cape Province in the South, then successively forms, in order from south to north,
405-523: Is the largest private reserve adjoining the World Heritage Site and is found in the accessible Kamberg area, the heart of the historic San (Bushman) painting region of the Ukhahlamba. The grassland of the lower slopes has been greatly affected by agriculture, however, especially by overgrazing . Nearly all of the original grassland and forest has disappeared and more protection is needed, although
450-552: Is unknown. The KwaZulu-Natal – Free State Drakensberg are composed of softer rocks and therefore have a more rounded, softer appearance from below. Generally, the top of the escarpment is almost table-top flat and smooth, even in Lesotho. The "Lesotho Mountains" are formed away from the Drakensberg escarpment by erosion gulleys which turn into deep valleys containing tributaries of the Orange River . The large number of such tributaries give
495-561: The Blyde and present-day Zandspruit rivers. On 5 May 1848, Joubert officially registered the farm at the land office in Ohrigstad , granting Hoedspruit its first recognition and registration as a town and municipality. In the 1850s, Ohrigstad grew into the central town of the area, but only older settlers were permitted to live in and around Ohrigstad itself. Younger settlers under the age of 45 were encouraged to move farther away. Consequently,
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#1733084550398540-588: The Drakensberg montane grasslands, woodlands, and forests ecoregion. The mountains are rich in plant life, including a large number of species listed in the Red Data Book of threatened plants, with 119 species listed as globally endangered and "of the 2 153 plant species in the park, a remarkable 98 are endemic or near-endemic". The flora of the high alti-montane grasslands is mainly tussock grass , creeping plants, and small shrubs such as ericas . These include
585-572: The Giant's Castle reserve is a haven for the eland and also is a breeding ground for the bearded vulture . 5.81% of the Drakensberg montane grasslands, woodlands and forests ecoregion is in protected areas. These include Kruger National Park , Mountain Zebra National Park , Golden Gate Highlands National Park, Camdeboo National Park , Sehlabathebe National Park, and Tsehlanyane National Park. The Maloti-Drakensberg Transfrontier Conservation Area
630-520: The Lesotho Highlands a very rugged mountainous appearance, both from the ground and from the air. The higher parts of Drakensberg have a mildly periglacial environment . It is possible that recent climate change has diminished the intensity of periglaciation. Knight and Grab mapped out the distribution of lightning strikes in the Drakensburg and discovered that lightning significantly controls
675-517: The Magaliesberg . The high treeless peaks of the Drakensberg (from 2,500 m (8,200 ft) upward) have been described by the World Wide Fund for Nature as the Drakensberg alti-montane grasslands and woodlands ecoregion . These steep slopes are the most southerly high mountains in Africa, and being farther from the equator provide cooler habitats at lower elevations than most mountain ranges on
720-462: The railway line from Tzaneen to Kaapmuiden . The Stone Age artifacts and sites from all three periods suggest continuous use by early humans. Early and Middle Iron Age sites near Hoedspruit have been excavated on the Happyland farm, dating between AD 450 and 1000. Dawid Johannes Joubert became the initial owner of Hoedspruit farm, acquiring the land in 1844 and settling in the region between
765-654: The uKhahlamba Drakensberg Park was listed by UNESCO in 2000 as a World Heritage site. The park also is in the List of Wetlands of International Importance (under the Ramsar Convention ). The Royal Natal National Park , which contains some of the higher peaks, is part of this large park complex. Adjacent to the Ukhahlamba Drakensberg World Heritage Site is the 1900 ha Allendale Mountain Reserve, which
810-797: The Drakensberg Royal Natal National Park and Bushman's Nek. Due to the materials used in their production, these paintings are difficult to date, but there is anthropological evidence, including many hunting implements, that the San people existed in the Drakensberg at least 40,000 years ago, and possibly more than 100,000 years ago. According to mountainsides.co.za, "[i]n Nd edema Gorge in the Central Ginsberg 3,900 paintings have been recorded at 17 sites. One of them, Sebaayeni Cave, contains 1,146 individual paintings." The website, south Africa.info, indicates that although "the oldest painting on
855-476: The Drakensberg are an essential resource for South Africa's economy, providing water for the industrial provinces of Mpumalanga and Gauteng , which contains the city of Johannesburg . The climate is wet and cool at the high elevations, which experience snowfall in winter. The grassy lower slopes (from 1,800 to 2,500 m (5,900 to 8,200 ft)) of the Drakensberg in Eswatini , South Africa and Lesotho constitute
900-511: The Drakensberg, two of which are highly venomous. One bird is endemic to the high peaks, the mountain pipit (Anthus hoeschi) , and another six species are found mainly here: Bush blackcap (Lioptilus nigricapillus) , buff-streaked chat (Oenanthe bifasciata) , Rudd's lark (Heteromirafra ruddi) , Drakensberg rockjumper (Chaetops aurantius) , yellow-breasted pipit (Anthus chloris) , and Drakensberg siskin (Serinus symonsi) . The endangered Cape vulture and lesser kestrel are two of
945-532: The European land surveyors assigned European names of cities, states, and countries to the official farms they were formalizing. As a result, the area is now populated with farms bearing names such as Essex, Madrid, Berlin, Richmond, Chester, Moscow, Dublin, Dundee, and Fife. Due to its proximity to private game reserves and the Kruger National Park , ecotourism and big game hunting are major contributor to
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#1733084550398990-793: The Land Office in Ohrigstad was extensive, stretching from the Blyde River to the Klaserie River and encompassing the present-day town center. Around the same time, a dispute arose between the Portuguese in Lourenço Marques (Maputo) and the South Africans in the Transvaal Republic over the international border near the Drakensberg mountain range behind Hoedspruit. The Portuguese claimed it was
1035-466: The Reserve is funded by means of a number of up-market private commercial game lodges located within the Reserve. They are involved in different kind of projects such as supporting local community through contributions to surrounding schools and sustainable farming . Thornybush Game Reserve shares an unfenced border with the Kruger National Park, which means that animals can move freely between
1080-452: The Transvaal Republic, President Kruger instructed the surveyors to mark the farm boundaries along the Drakensberg mountains before their return to Europe , as the region was gaining attention for potential settlement opportunities. The large farms, including the original Hoedspruit farm, were divided into smaller registered farms, still owned and operated by a single farmer. With limited knowledge of local cultures, languages, and customs,
1125-622: The area bordering on Lesotho, which contains an area popular for hikers, Cathedral Peak . North of Lesotho the range becomes lower and less rugged until entering Mpumalanga where the quartzite mountains of the Transvaal Drakensberg are loftier and more broken and they form the eastern rim of the Transvaal Basin, the Blyde River Canyon lying within this stretch. The geology of this section is the same as, and continuous with, that of
1170-419: The birds of prey that hunt in the mountains. Mammals include klipspringer (Oreotragus oreotragus) , eland (Taurotragus oryx) , and mountain reedbuck (Redunca fulvorufula) . Other endemic species include three frogs found in the mountain streams, Drakensberg river frog (Amietia dracomontana) , Phofung river frog ( Amietia vertebralis ) , and Maluti river frog (Amietia umbraculata) . Fish are found in
1215-603: The border between Lesotho and the Eastern Cape and the border between Lesotho and KwaZulu-Natal Province . Thereafter it forms the border between KwaZulu-Natal and the Free State , and next as the border between KwaZulu-Natal and Mpumalanga Province . The escarpment winds north from there, through Mpumalanga, where it includes features such as the Blyde River Canyon , Three Rondavels , and God's Window . It then extends farther north to Hoedspruit in southeastern Limpopo where it
1260-605: The border between Mozambique and South Africa, while the South Africans argued it was the Lebombo Mountains . To settle the matter, President Oom Paul Kruger of the Transvaal Republic ordered a proper land survey study to determine the official border. Since there were no qualified land surveyors in South Africa then, three main surveyors were brought in from Europe, including Von Weilligh, Vos, and Gillfillan. While in
1305-518: The continent. High rainfall generates many mountain streams and rivers, including the sources of the Orange River , southern Africa's longest, and the Tugela River . These mountains also have the world's highest waterfall, the Tugela Falls (Thukela Falls), which has a total drop of 947 m (3,107 ft) (Venezuela's Angel Falls is also a candidate for highest waterfall). The rivers that run from
1350-570: The easily eroded sandstone of Clarens Formation , the layer below the thick, hard basalt layer on the KwaZulu Natal-Lesotho border. Many of these caves have paintings by the San (Bushmen). This portion of the Drakensberg has between 35,000 and 40,000 works of San rock art , and is the largest collection of such parietal work in the world. Some 20,000 individual rock paintings have been recorded at 500 different caves and overhanging sites between
1395-411: The east, with the result that most of the plateau lies above 1,000 m (3,300 ft) despite extensive erosion. The plateau is tilted such that it is highest in the east and slopes gently downward toward the west and south. Typically, the elevation of the edge of the eastern escarpments is in excess of 2,000 m (6,600 ft). It reaches its highest point of over 3,000 m (9,800 ft) where
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1440-711: The environment is fairly undamaged. However, tourism in the Drakensberg is developing, with a variety of hiking trails , hotels, and resorts appearing on the slopes. Much of the higher South African parts of the range have been designated as game reserves or wilderness areas . 7% of the Drakensberg alti-montane grasslands and woodlands ecoregion is in protected areas. These include Golden Gate Highlands National Park , Sehlabathebe National Park , Tsehlanyane National Park , Malekgalonyane Nature Reserve , Giant's Castle Game Reserve , Loteni Nature Reserve , Natal National Park , Vergelegen Nature Reserve , Beaumont Nature Reserve , and Lammergeier Highlands Nature Reserve . Of these
1485-620: The escarpment forms part of the international border between Lesotho and the South African province of KwaZulu-Natal . The escarpment seen from below resembles a range of mountains. The Limpopo, Mpumalanga, and Lesotho Drakensberg have hard erosion-resistant upper surfaces and therefore have a very rugged appearance, combining steep-sided blocks and pinnacles (giving rise to the Zulu name "Barrier of up-pointed spears"). Who first gave these mountains their Afrikaans or Dutch name Drakensberg , and why,
1530-499: The evolution of the mountain landscapes because it helps to shape the summit areas – the highest areas – with this blasting effect. Previously, angular debris was presumed to have been created by changes typical of cold, periglacial environments, such as fracturing due to frost. The geological composition of Drakensberg (escarpment wall) varies considerably along its more than 1000 km length. The Limpopo and Mpumalanga Drakensberg are capped by an erosion resistant quartzite layer that
1575-422: The highest part of Drakensberg the composition of the flora is independent on slope aspect (direction) and varies, depending on the hardness of the rock clasts . This hardness is related to weathering and is variable even within a single landform . The Drakensberg area is "home to 299 recorded bird species"' making up "37% of all non-marine avian species in southern Africa". There are 24 species of snakes in
1620-588: The local economy. Agriculture is the other major regional industry focusing on citrus and mango production. Air Force Base Hoedspruit is home to 19 Squadron , South African Air Force helicopter unit. The civil Eastgate Airport , which shares the Air Force base's airfield, is served by several charter operators. This Limpopo location article is a stub . You can help Misplaced Pages by expanding it . Drakensberg Mountains The Drakensberg ( Zulu : uKhahlamba, Sotho : Maloti, Afrikaans : Drakensberge)
1665-583: The many rivers and streams, including the Maluti redfin ( Pseudobarbus quathlambae ) that was thought to be extinct before being found in the Senqunyane River in Lesotho. The lower slopes of the Drakensberg support much wildlife, perhaps most importantly the rare southern white rhinoceros (which was nurtured here when facing extinction) and the black wildebeest ( Connochaetes gnou , which as of 2011 only thrives in protected areas and game reserves). The area
1710-620: The name the earliest Dutch settlers gave to the escarpment, namely Drakensbergen , or Dragons' Mountains . The highest portion of the Great Escarpment is known in Zulu as uKhahlamba and as Maloti in Sotho ("Barrier of up-pointed spears"). The Great Escarpment is composed of steep rift valley walls formed around a bulging of continental crust during the breakup of southern Gondwana that have since eroded inland from their original positions near
1755-920: The northeastern and eastern borders of Lesotho, as well as the Eastern Cape Drakensberg, are composed of a thick layer of basalt (lava) that erupted 180 million years ago. That layer rests on the youngest of the Karoo Supergroup sediments, the Clarens sandstone , which was laid down under desert conditions, about 200 million years ago. The highest peak is Thabana Ntlenyana , at 3,482 m (11,424 ft). Other notable peaks include Mafadi (3,450 m (11,319 ft)), Makoaneng at 3,416 metres (11,207 ft), Njesuthi at 3,408 metres (11,181 ft), Champagne Castle at 3,377 metres (11,079 ft), Giant's Castle at 3,315 metres (10,876 ft), Ben Macdhui at 3,001 metres (9,846 ft), and Popple Peak at 3,331 metres (10,928 ft), all of these are in
1800-405: The periphery of the original Hoedspruit farm. The name "Hoedspruit" was given by Dawid Johannes Joubert himself after a significant incident in 1844 when a severe cloud burst caused the river, now known as Zandspruit, to flood rapidly. During the event, Joubert lost his hat in the raging river. Given that a hat was a valuable resource for a farmer in those times, serving various purposes, losing it
1845-600: The rare Spiral Aloe ( Aloe polyphylla ) , which as its name suggests, has leaves with a spiral shape. Meanwhile, the lower slopes are mainly grassland, but are also home to conifers , which are rare in Africa, the species of conifer found in the Drakensberg belong to the genus Podocarpus . The grassland is of interest as it contains a great number of endemic plants. Grasses found here include oat grass Monocymbium ceresiiforme , Diheteropogon filifolius , Sporobolus centrifugus , caterpillar grass ( Harpochloa falx ) , Cymbopogon dieterlenii , and Eulalia villosa . In
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1890-557: The reserve and the park. The wildlife counts: There are in total 12 different places to stay in Thornybush Game Reserve: Premium Collection ;: Classic Collection : Hoedspruit Hoedspruit ( Afrikaans for Hat Creek ) is a town situated at the foot of the Klein Drakensberg (Afrikaans for "Small Dragon Mountains" range), in the Limpopo province of South Africa , on
1935-465: The southern African coast, and its entire eastern portion (see the accompanying map) constitutes the Drakensberg. The Drakensberg terminate in the north near Tzaneen at about the 22° S parallel. The absence of the Great Escarpment for approximately 450 km (280 mi) to the north of Tzaneen (to reappear on the border between Zimbabwe and Mozambique in the Chimanimani Mountains )
1980-464: Was a major event for Joubert. Consequently, he named the river "Hoedspruit," meaning "Hat River/stream/creek" in reference to the river that took his hat. Dawid Johannes Joubert owned another farm in the Ohrigstad area and split his time between both farms. Sadly, in 1860, he was killed by a leopard while on his farm in Ohrigstad. During Joubert's ownership, the Hoedspruit farm that he registered with
2025-485: Was established to preserve some of the high mountain areas of the range. Towns and cities in the Drakensberg area include, from south to north, Matatiele and Barkly East in the Eastern Cape Province; Ladysmith , Newcastle , Ulundi – the former Zulu capital, Dundee , and Ixopo in KwaZulu-Natal; all of Lesotho, whose capital is Maseru ; and Tzaneen in Limpopo Province . There are numerous caves in
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