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By the way, we would recommend you to combine your visit to Drakensberg with other popular and interesting places of South Africa, for example: Johannesburg, Potchefstroom, Pretoria, Mossel Bay, Bloemfontein, Sandton, East London, Stellenbosch, Knysna, George, Polokwane, Umhlanga, Durban, Drakensberg, Rustenburg, Kempton Park, Benoni, Pietermaritzburg, Kruger National Park, Plettenberg Bay, Kimberley, Boksburg, Port Elizabeth, Marloth Park, Ballito, Nelspruit, etc.
How to Book a Hotel in Drakensberg
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Hotels of Drakensberg
A hotel in Drakensberg is an establishment that provides lodging paid on a short-term basis. Facilities provided may range from a basic bed and storage for clothing, to luxury features like en-suite bathrooms. Larger in Drakensberg hotels may provide additional guest facilities such as a swimming pool, business centre, childcare, conference facilities and social function services. Hotel rooms in Drakensberg are usually numbered (or named in some smaller hotels and B&Bs) to allow guests to identify their room. Some Drakensberg hotels offer meals as part of a room and board arrangement. Hotel operations vary in size, function, and cost. Most Drakensberg hotels and major hospitality companies that operate hotels in Drakensberg have set widely accepted industry standards to classify hotel types. General categories include the following:
Upscale luxury hotels in Drakensberg
An upscale full service hotel facility in Drakensberg that offers luxury amenities, full service accommodations, on-site full service restaurant(s), and the highest level of personalized and professional service. Luxury Drakensberg hotels are normally classified with at least a Four Diamond or Five Diamond status or a Four or Five Star rating depending on classification standards.
Full service hotels in Drakensberg
Full service Drakensberg hotels often contain upscale full-service facilities with a large volume of full service accommodations, on-site full service restaurant(s), and a variety of on-site amenities such as swimming pools, a health club, children's activities, ballrooms, on-site conference facilities, etc.
Historic inns and boutique hotels in Drakensberg
Boutique hotels of Drakensberg are smaller independent non-branded hotels that often contain upscale facilities of varying size in unique or intimate settings with full service accommodations. Drakensberg boutique hotels are generally 100 rooms or less. Some historic inns and boutique hotels in Drakensberg may be classified as luxury hotels.
Focused or select service hotels in Drakensberg
Small to medium-sized hotel establishments that offer a limited amount of on-site amenities that only cater and market to a specific demographic of Drakensberg travelers, such as the single business traveler. Most Drakensberg focused or select service hotels may still offer full service accommodations but may lack leisure amenities such as an on-site restaurant or a swimming pool.
Economy and limited service hotels in Drakensberg
Small to medium-sized Drakensberg hotel establishments that offer a very limited amount of on-site amenities and often only offer basic accommodations with little to no services, these facilities normally only cater and market to a specific demographic of travelers, such as the budget-minded Drakensberg traveler seeking a "no frills" accommodation. Limited service Drakensberg hotels often lack an on-site restaurant but in return may offer a limited complimentary food and beverage amenity such as on-site continental breakfast service.
Guest houses and B&Bs in Drakensberg
A bed and breakfast in Drakensberg is a small lodging establishment that offers overnight accommodation and inclusive breakfast. Usually, Drakensberg bed and breakfasts are private homes or family homes offering accommodations. The typical Drakensberg B&B has between 4 and 11 rooms, with 6 being the average. Generally, guests are accommodated in private bedrooms with private bathrooms, or in a suite of rooms including an en suite bathroom. Some homes have private bedrooms with a bathroom which is shared with other guests. Breakfast is served in the bedroom, a dining room, or the host's kitchen. Often the owners of guest house themselves prepare the breakfast and clean the rooms.
Hostels in Drakensberg
Drakensberg hostels provide budget-oriented, sociable accommodation where guests can rent a bed, usually a bunk bed, in a dormitory and share a bathroom, lounge, and sometimes a kitchen. Rooms can be mixed or single-sex, although private rooms may also be available. Hostels are often cheaper for both the operator and occupants; many Drakensberg hostels have long-term residents whom they employ as desk agents or housekeeping staff in exchange for experience or discounted accommodation.
Apartment hotels, extended stay hotels in Drakensberg
Extended stay hotels are small to medium-sized Drakensberg hotels that offer longer term full service accommodations compared to a traditional hotel. Extended stay hotels may offer non-traditional pricing methods such as a weekly rate that cater towards travelers in need of short-term accommodations for an extended period of time. Similar to limited and select service hotels, on-site amenities are normally limited and most extended stay hotels in Drakensberg lack an on-site restaurant.
Timeshare and destination clubs in Drakensberg
Drakensberg timeshare and destination clubs are a form of property ownership also referred to as a vacation ownership involving the purchase and ownership of an individual unit of accommodation for seasonal usage during a specified period of time. Timeshare resorts in Drakensberg often offer amenities similar that of a Full service hotel with on-site restaurant(s), swimming pools, recreation grounds, and other leisure-oriented amenities. Destination clubs of Drakensberg on the other hand may offer more exclusive private accommodations such as private houses in a neighborhood-style setting.
Motels in Drakensberg
A Drakensberg motel is a small-sized low-rise lodging establishment similar to that of a limited service hotel, but with direct access to individual rooms from the car park. Common during the 1950s and 1960s, motels were often located adjacent to a major road, where they were built on inexpensive land at the edge of towns or along stretches of highways. They are still useful in less populated areas of Drakensberg for driving travelers, but the more populated an area becomes the more hotels fill the need. Many of Drakensberg motels which remain in operation have joined national franchise chains, rebranding themselves as hotels, inns or lodges.
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The Drakensberg (Afrikaans: Drakensberge, isiZulu: uKhahlamba, SeSotho: Maluti) is the name given to the eastern portion of the Great Escarpment, which encloses the central Southern African plateau. The Great Escarpment reaches its greatest elevation in this region – 2,000 to 3,000 metres (6,600 to 9,800 feet).
A map of South Africa showing the central plateau edged by the Great Escarpment and its relationship to the Cape Fold Mountains to the south. The portion of the Great Escarpment shown in red is known as the Drakensberg.
The Drakensberg escarpment stretches for over 1,000 kilometres (600 miles) from the Eastern Cape Province in the South, then successively forms, in order from south to north, 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. It winds north, through Mpumalanga, where it includes features such as the Blyde River Canyon, Three Rondavels and God's Window. It moves north again above Tzaneen in Limpopo Province, where it includes the Wolkberg Mountains and Iron Crown Mountain, at 2,200 m (7,200 ft) above sea level, the Wolkberg being the highest mountain range in Limpopo. It veers west again and at Mokopane it is known as the Strydpoort Mountains.
The Afrikaans name Drakensberge comes from the name the earliest Dutch settlers to the region gave it. They called them the Drakensbergen, or "Mountains of Dragons". Several possible reasons for this name include the pointy tops giving an appearance similar to that of the back of the mythical European dragon, old local myths of dragons roaming the mountains, and possible findings of dinosaur fossils (which would have been confused with the remains of dragons).
When most South Africans and visitors speak of the Drakensberg, they refer to the Great Escarpment that forms the border between Lesotho and KwaZulu-Natal, believing it to be a range of mountains extending into Lesotho, more correctly known as the Lesotho Highlands. (This narrow use of the name "Drakensberg" is analogous to the use of the name "America" to refer to just the United States of America, rather than to the continent in which the United States is situated.) This highest portion of the Great Escarpment is known as uKhahlamba ("Barrier of up-pointed spears") in Zulu and Maluti in Sotho.
Drakensberg: Geological origins
About 180 million years ago, a mantle plume under southern Gondwana caused bulging of the continental crust in the area that would later become southern Africa. Within 10–20 million years rift valleys formed on either side of the central bulge, which became flooded to become the proto-Atlantic and proto-Indian oceans. The stepped steep walls of these rift valleys formed escarpments that surrounded the newly formed Southern African subcontinent. With the widening of the Atlantic, Indian and Southern oceans, Southern Africa became tectonically quiescent. Earthquakes rarely occur, and there has been no volcanic or orogenic activity for about 50 million years. An almost uninterrupted period of erosion has continued to the present, resulting in layers several kilometers thick having been lost from the surface of the plateau. A thick layer of marine sediment was consequently deposited onto the continental shelf (the lower steps of the original rift valley walls) which surrounds the subcontinent.
During the past 20 million years, further massive upliftment, especially in the East, has taken place in Southern Africa. As a result, most of the plateau lies above 1,000 m (3,300 ft) despite the extensive erosion. The plateau is tilted such that its highest point is in the east, and it slopes gently downwards towards the west and south. The elevation of the edge of the eastern escarpments is typically in excess of 2,000 m (6,600 ft). It reaches its highest point (over 3,000 m (9,800 ft)) where the escarpment forms part of the international border between Lesotho and the South African province of KwaZulu-Natal.
The upliftment of the central plateau over the past 20 million years and erosion resulted in the original escarpment being moved inland, creating the present-day coastal plain. The position of the present escarpment is approximately 150 km inland from the original fault lines which formed the walls of the rift valley that developed along the coast during the break-up of Gondwana. The rate of the erosion of the escarpment in the Drakensberg region is said to average 1.5 m (5 ft) per 1000 years, or 1.5 millimetres (⁄16 in) per year.
Because of the extensive erosion of the plateau, which occurred over most of the Mesozoic and Cenozoic eras, none of its surface rocks (except the Kalahari sands) are younger than 180 million years. The youngest rocks that remain cap the plateau in Lesotho. These are the Clarens Formation laid down under desert conditions about 200 million years ago, topped by a 1,600 m (5,200 ft) thick layer of lava which erupted, and covered most of Southern Africa, and large parts of Gondwana, about 180 million years ago. These rocks form the steep sides of the Great Escarpment in this region, where its upper edge reaches an elevation in excess of 3,000 m (9,800 ft).
The erosional retreat of the escarpment from the coast to its present position, means that the rocks of the coastal plain are, with very few and small exceptions, older than those that cap the top of the escarpment. Thus the rocks of the Mpumalanga Lowveld below the Mpumalanga portion of the Great Escarpment are more than 3000 million years old. The rocks of the KwaZulu-Natal Midlands belong, in the main, to the Beaufort and Ecca Groups (of the Karoo Supergroup), aged 220-310 million years, and are therefore considerably older than the Drakensberg lavas (aged 180 million years) which cap the escarpment on the border between KwaZulu-Natal and Lesotho.
The entire eastern portion of the Great Escarpment (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 about 450 km (280 mi) to the north of Tzaneen (to reappear on the border between Zimbabwe and Mozambique in the Chimanimani Highlands) 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 Low veld.
An approximate SW-NE cross section through South Africa with the Cape Peninsula (with Table Mountain) on the far left, and north-eastern KwaZulu-Natal on the right. Diagrammatic and only roughly to scale. It shows how the Drakensberg Escarpment is related to the major geographical features that dominate the southern and eastern parts of the country, particularly the Central Plateau, whose south-western edge (in the diagram) is called the Roggeberg escarpment (not labelled). The major geological layers that shape this geography are indicated in different colors, whose significance and origin are explained under the headings "Karoo Supergroup" and "Cape Supergroup". The 1600 m thick layer of hard, erosion-resistant basalt (lava) that accounts for the height and steepness of the Drakensberg Escarpment on the KwaZuluNatal-Lesotho border is indicated in blue. Immediately below it is the Stormberg Group shown in green. The Clarence Formation with its numerous caves and San rock paintings, forms part of this latter group.
The escarpment seen from below looks like 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, is unknown.). The KwaZulu-Natal - Free State Drakensberg are composed of softer rocks and therefore have a more rounded, softer appearance from below. The top of the escarpment is generally 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 which contain tributaries of the Orange River. The large number of tributaries give the Lesotho Highlands a very rugged mountainous appearance, both from the ground and from the air.
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 which 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, which are 300 million years old. The portion of the Drakensberg that forms the KwaZulu-Natal – Free State border is formed by slightly younger Beaufort rocks (250 million years old) which are also part of the Karoo Supergroup. The Ecca and Beaufort groups are composed of sedimentary rocks which are less erosion resistant than the other rocks which make up the Drakensberg escarpment. This portion of escarpment is therefore not as impressive as the Mpumalanga and Lesotho stretches of the Drakensberg. The Drakensberg which form the north-eastern and eastern borders of Lesotho, as well as the Eastern Cape Drakensberg are composed of a thick layer of basalt (lava) which erupted 180 million years ago. That rests on the youngest of the Karoo Supergroup sediments, the Clarens sandstone, which was laid down under desert conditions, about 200 million years ago.
Drakensberg: Highest peaks
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 m, Njesuthi at 3,408 m, Champagne Castle at 3,377 m, Giant's Castle at 3,315 m, Ben Macdhui at 3,001 m, and Popple Peak at 3331m, all of these are in the area bordering on Lesotho. Another popular area for hikers is 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 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 the Magaliesberg.
Drakensberg: Mountain passes
Main article: List of mountain passes of KwaZulu-Natal
Tugela Falls vicinity – Tugela River in valley
The high treeless peaks of the Drakensberg (from 2,500 m (8,200 ft) upwards) have been described by the World Wildlife Fund as the Drakensberg alti-montane grasslands and woodlands ecoregion. These steep slopes are the most southerly high mountains in Africa, and being further from the equator provide cooler habitats at lower elevations than most mountain ranges on the continent. The 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 second-highest waterfall, the Tugela Falls (Thukela Falls), which has a total drop of 947 m (3,107 ft). The rivers that run from 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.
Meanwhile, the grassy lower slopes (from 1,800 to 2,500 m (5,900 to 8,200 ft)) of the Drakensberg in Swaziland, South Africa and Lesotho constitute the Drakensberg Montane Grassland, Woodland, and Forest.
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 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 is Podocarpus. The grassland itself 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.
The Drakensberg area is "home to 299 recorded bird species"' making up "37% of all non-marine avian species in southern Africa."
Drakensberg: Fauna of the high peaks
There is one bird that is endemic to the high peaks, the mountain pipit (Anthus hoeschi), while another six 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 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 the many rivers and streams including the Maluti redfin (Pseudobarbus quathlambae), which was thought to be extinct but has been found in the Senqunyane River in Lesotho.
Drakensberg: Fauna of the lower slopes
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 is home to large herds of grazing 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 are also present. Endemic species include a large number of chameleons and other reptiles. There is one endemic frog, forest rain frog (Breviceps sylvestris), and four more 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).
A view of the Mpumalanga Drakensberg portion of the Great Escarpment, from God's Window, near Graskop looking south. The hard erosion resistant layer that forms the upper edge of the escarpment here consists of flat lying quartzite belonging to the Black Reef Formation, which also forms the Magaliesberg mountains near Pretoria.
The high slopes are hard to reach so 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. Most of the higher South African parts of the range have been designated as game reserves or wilderness areas. Of these the UKhahlamba / Drakensberg Park was listed by UNESCO in 2000 as a World Heritage site. The park is also 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 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 meanwhile has been greatly affected by agriculture, especially overgrazing. Original grassland and forest has nearly all disappeared and more protection is needed, though the Giant's Castle reserve is a haven for the eland and also is a breeding ground for the bearded vulture.
Panorama of the Giant's Castle region
The Maloti-Drakensberg Transfrontier Conservation Area was established to preserve some of the high mountain areas of the range.
Drakensberg: Urban areas
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.
Drakensberg: San cave paintings
San rock painting of an eland in a Clarens Formation cave in the UKhahlamba Drakensberg Park of KwaZulu-Natal close to the Lesotho border.
There are numerous caves in 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 rock paintings by the San (Bushmen). This portion of the Drakensberg has between 35000 and 40000 works of San rock art and is the largest collection of such work in the world. Some 20,000 individual rock paintings have been recorded at 500 different caves and overhanging sites between 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 over 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 though "the oldest painting on a rock shelter wall in the Ginsberg dates back about 2400 years.....paint chips at least a thousand years older have also been found." The site also indicates that "[t]he rock art of the Drakensberg is the largest and most concentrated group of rock paintings in Africa south of the Sahara, and is outstanding both in quality and diversity of subject."
Drakensberg: In popular culture
Drakesberg was featured on the 2009 American science fiction movie 2012. It was mentioned in the last scene of the movie whereby after twenty-seven days of a great flood which people tried to survive by building arks, the waters are receding. The arks approach the Cape of Good Hope, where the Drakensberg (now the tallest mountain range on Earth) is emerging.
Drakensberg: See also
List of mountains in South Africa
Atlas of Southern Africa(1984). p. 13, 190-192. Readers Digest Association, Cape Town
Encyclopædia Britannica (1975); Micropaedia Vol. III, p. 655. Helen Hemingway Benton Publishers, Chicago.
Pearse, R.O. (1973) Barrier of Spears. Drama of the Drakensberg. p. i. Howard Timmins, Epping, Cape
McCarthy, T. & Rubidge, B. (2005). The Story of Earth and Life. pp. 16-7,192-195, 245-248, 263, 267-269. Struik Publishers, Cape Town.
Truswell, J.F. (1977). The Geological Evolution of South Africa. pp. 151-153,157-159,184–188, 190. Purnell, Cape Town.
Encyclopædia Britannica (1975); Macropaedia, Vol. 17. p. 60. Helen Hemingway Benton Publishers, Chicago.
Atlas of Southern Africa. (1984). Readers Digest Association, Cape Town
McCarthy, T.S. (2013) "The Okavango delta and its place in the geomorphological evolution of Southern Africa," South African Journal of Geology 116: 1-54.
Norman, n. & Whitfield, G. (2006). Geological Journeys. p.290-300. Struik Publishers, Cape Town.
Geological map of South Africa, Lesotho and Swaziland (1970). Council for Geoscience, Geological Survey of South Africa.
Sycholt, August (2002). Roxanne Reid, ed. A Guide to the Drakensberg. Cape Town: Struik Publishers. p. 9. ISBN 1-86872-593-6.
The Times comprehensive atlas of the World. (1999) p. 90. Times Books Group, London.
"Drakensberg alti-montane grasslands and woodlands". Terrestrial Ecoregions. World Wildlife Fund.
Alexander, Mary. "Drakensberg: Barrier of Spears". Retrieved 2008-10-03.
A Complete Guide to the southern African Frogs. Louis du Preez and Vincent Carruthers
Maloti-Drakensberg Transfrontier Conservation Area
"Bushman and San Paintings in the Drakensberg". Drakensberg Tourism. Retrieved 2008-10-03.
"Drakensberg Rock Art". Retrieved 2008-10-03.
https://web.archive.org/web/20080525110813/.Missing or empty |title= (help)
Rosen, Deborah; Lewis, Colin; Illgner, Peter (1999). "Palaeoclimatic And Archaeological Implications of Organic- Rich Sediments at Tifftidell Ski Resort, Near Rhodes, Eastern Cape Province, South Africa". Transactions of the Royal Society of South Africa. 54 (2): 311–321. doi:10.1080/00359199909520630.
Drakensberg: External links
Mpumalanga Escarpment in a weekend travel guide from Wikivoyage
Wikimedia Commons has media related to Drakensberg.
Wikisource has the text of the 1921 Collier's Encyclopedia article Drakenberge.
Wikivoyage has a travel guide for Ukhahlamba Drakensberg.
KZN Drakensberg Homepage – Official Website for the KwaZulu Natal Drakensberg.
Nature – Drakensberg: Barrier of Spears – PBS Nature episode covering the eland (largest member of antelope family) of the Drakensberg.
Drakensberg hiking trails
Major African geological formations
Cratons and shields
West African Craton
Broodkop Shear Zone
Central African Shear Zone
Chuan Shear Zones
Foumban Shear Zone
Mwembeshi Shear Zone
Todi Shear Zone
Western Meseta Shear Zone
Cape Fold Belt
East African Orogen
Terra Australis Orogen
Bahr el Arab rift
Blue Nile rift
East African Rift
Gulf of Suez Rift
Red Sea Rift
White Nile rift
Blue Nile Basin
Foreland Karoo Basin
Niger Delta Basin
Orange River basin
Ouled Abdoun Basin
Rio del Rey Basin
Somali Coastal Basin
Tanzania Coastal Basin
Central Pangean Mountains
East African mountains
Great Karas Mountains
Serra da Leba
Serra da Chela
World Heritage Sites in South Africa
For official site names, see each article or the List of World Heritage Sites in South Africa.
Cape Floral Region Protected Areas
Fossil Hominid Sites of South Africa
Cradle of Humankind
iSimangaliso Wetland Park
Mapungubwe Cultural Landscape
Richtersveld Cultural and Botanical Landscape
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