96-497: The Drakensberg ( Zulu : uKhahlamba, Sotho : Maloti, Afrikaans : Drakensberge) 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
192-399: A homorganic nasal consonant (so-called "prenasalisation", described in more detail below) and optionally followed by the consonant /w/ . In addition, syllabic /m̩/ occurs as a reduction of former /mu/ , and acts like a true syllable: it can be syllabic even when not word-initial, and can also carry distinctive tones like a full syllable. It does not necessarily have to be homorganic with
288-606: A velar fricative in place of the alveolar click , Groote River (derived from Kai !Garib ) or Senqu River (used in Lesotho), derived from ǂNū "Black". It is known in isiZulu as isAngqu. The Orange rises in the Drakensberg mountains along the border between South Africa and Lesotho, about 193 km (120 mi) west of the Indian Ocean and at an altitude of over 3,000 m (9,800 ft). The extremity of
384-424: A breathy consonant syllable, like dla , are [ɮǎ̤ ɮa̤᷈ ɮà̤] . A depressor does not affect a syllable that's already low, but it blocks assimilation to a preceding high tone so that the tone of the depressor syllable and any following low-tone syllables stays low. Prenasalisation occurs whenever a consonant is preceded by a homorganic nasal, either lexically or as a consequence of prefixation. The most notable case of
480-408: A high-tone syllable and another tonic syllable assimilates to that high tone. That is, if the preceding syllable ends on a high tone and the following syllable begins with a high tone (because it is high or falling), the intermediate toneless syllable has its pitch raised as well. When the preceding syllable is high but the following is toneless, the medial toneless syllable adopts a high-tone onset from
576-437: A labial consonant plus /w/ . Whenever /w/ follows a labial consonant, it changes to /j/ , which then triggers palatalization of the consonant. This effect can be seen in the locative forms of nouns ending in -o or -u , which change to -weni and -wini respectively in the locative. If a labial consonant immediately precedes, palatalization is triggered. The change also occurs in nouns beginning in ubu- with
672-597: A lion, Father ) and Siyonqoba (English: We will conquer ) was used. In some movie songs, like "This Land", the voice says Busa leli zwe bo ( Rule this land ) and Busa ngothando bo ( Rule with love ) were used too. The song Siyahamba is a South African hymn originally written in the Zulu language that became popular in North American churches in the 1990s. The remix of the 2019 worldwide hit Jerusalema contains lyrics in Zulu language. Standard Zulu as it
768-417: A lowering effect on pitch, adding a non-phonemic low-tone onset to the normal tone of the syllable. Thus, in syllables with depressor consonants, high tones are realised as rising, and falling tones as rising-then-falling. In both cases, the pitch does not reach as high as in non-depressed syllables. The possible tones on a syllable with a voiceless consonant like hla are [ɬá ɬâ ɬà] , and the possible tones of
864-598: 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 the Lesotho Highlands a very rugged mountainous appearance, both from
960-550: A natural pipe through which the diamonds gradually enter the river. Other sites said to be lairs of the creature include the pool beneath the King George Cataract at Aughrabies Falls , which is also said to be a source of diamonds, and a large rock in the middle of the river itself. In this version of the legend, the Grootslang is also said to prey on cattle from the river's banks. As the collection point for
1056-452: 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
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#17327662989411152-448: A result of word position as well. The remote demonstrative pronouns may appear with the suffix -ana when sentence-final, but only as -ā otherwise. Likewise, the recent past tense of verbs ends in -ile sentence-finally, but is reduced to -ē medially. Moreover, a falling tone can only occur on a long vowel, so the shortening has effects on tone as well. Some words, such as ideophones or interjections, can have stress that deviates from
1248-620: 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." Zulu language Zulu ( / ˈ z uː l uː / ZOO -loo ), or isiZulu as an endonym ,
1344-540: A stem beginning with a vowel. The following changes occur as a result of palatalization: Zulu employs the 26 letters of the ISO basic Latin alphabet . However, some of the letters have different pronunciations than in English. Additional phonemes are written using sequences of multiple letters. Tone, stress and vowel length are not indicated. Reference works and older texts may use additional letters. A common former practice
1440-537: A strong association with the history of colonial subjugation and has therefore no place under the current democratic dispensation." In South African folklore, the Orange River is often associated with the Grootslang , a mythical being resembling a giant serpent, which is often connected to the river's alluvial diamonds. The Grootslang is described as living in a gem-filled cave connected to the Orange River by
1536-694: Is a Southern Bantu language of the Nguni branch spoken and indigenous to Southern Africa . It is the language of the Zulu people , with about 13.56 million native speakers, who primarily inhabit the province of KwaZulu-Natal in South Africa . The word "KwaZulu-Natal" translates into English as "Home of the Zulu Nation is Natal". Zulu is the most widely spoken home language in South Africa (24% of
1632-399: Is a contraction of an earlier ilithambo /ílítʰámbó/ , which may still be used by some speakers. Likewise, uphahla /úːpʰaɬa/ "roof" is a contraction of the earlier uluphahla /ulúpʰaɬa/ . In addition, the vowel of the penultimate syllable is allophonically lengthened phrase- or sentence-finally. The use of click consonants is one of the most distinctive features of Zulu. This feature
1728-882: Is a river in Southern Africa . It is the longest river in South Africa . With a total length of 2,432 km (1,511 mi), the Orange River Basin extends from Lesotho into South Africa and Namibia to the north. It rises in the Drakensberg mountains in Lesotho, flowing westwards through South Africa to the Atlantic Ocean . The river forms part of the international borders between South Africa and Lesotho and between South Africa and Namibia, as well as several provincial borders within South Africa. Except for Upington , it does not pass through any major cities. The Orange River plays an important role in
1824-465: Is a sequence of high-low and occurs only on long vowels. The penultimate syllable can also bear a falling tone when it is long due to the word's position in the phrase. However, when it shortens, the falling tone becomes disallowed in that position. In principle, every morpheme has an inherent underlying tone pattern which does not change regardless of where it appears in a word. However, like most other Bantu languages, Zulu has word tone , meaning that
1920-815: Is a table with some words constructed from the roots - Zulu and -ntu (the root for person/people ): The following is a list of phrases that can be used when one visits a region whose primary language is Zulu: The following is from the preamble to the Constitution of South Africa : Thina, bantu baseNingizimu Afrika, Siyakukhumbula ukucekelwa phansi kwamalungelo okwenzeka eminyakeni eyadlula; Sibungaza labo abahluphekela ubulungiswa nenkululeko kulo mhlaba wethu; Sihlonipha labo abasebenzela ukwakha nokuthuthukisa izwe lethu; futhi Sikholelwa ekutheni iNingizimu Afrika ingeyabo bonke abahlala kuyo, sibumbene nakuba singafani. Orange River Quthing , The Orange River (from Afrikaans / Dutch : Oranjerivier )
2016-408: 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 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
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#17327662989412112-549: 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
2208-460: Is generally not navigable for long stretches. The river has a total length of 2,432 km (1,511 mi). In the dry season , the volume of the water in the river is considerably reduced because of the rapid run-off and evaporation . At the source of the Orange, the rainfall is about 2,000 mm (79 in) per annum, but precipitation decreases as the river flows westward; at its mouth,
2304-727: 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
2400-602: Is mostly predictable and normally falls on the penultimate syllable of a word. It is accompanied by an allophonic lengthening of the vowel. When the final vowel of a word is long due to contraction, it receives the stress instead of the preceding syllable. Lengthening does not occur on all words in a sentence, however, but only those that are sentence- or phrase-final. Thus, for any word of at least two syllables, there are two different forms, one with penultimate length and one without it, occurring in complementary distribution. In some cases, there are morphemic alternations that occur as
2496-418: Is often not understood by young people. The vowel system of Zulu consists of five vowels. /ɛ/ and /ɔ/ are pronounced [ e ] and [ o ], respectively, if the following syllable contains the [+ ATR ] vowels /i/ or /u/ . They are [ɛ] and [ɔ] otherwise: There is limited vowel length in Zulu, as a result of the contraction of certain syllables. For example, the word ithambo /íːtʰámbó/ "bone",
2592-668: 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
2688-502: Is shared with several other languages of Southern Africa, but it is very rare in other regions. There are three basic articulations of clicks in Zulu: Each articulation covers five click consonants, with differences such as being slack-voiced, aspirated or nasalised , for a total of 15. Zulu syllables are canonically (N)C(w)V , and words must always end in a vowel. Consonant clusters consist of any consonant, optionally preceded by
2784-442: Is taught in schools, also called "deep Zulu" ( isiZulu esijulile ), differs in various respects from the language spoken by people living in cities (Urban Zulu, isiZulu sasedolobheni ). Standard Zulu tends to be purist , using derivations from Zulu words for new concepts, whereas speakers of Urban Zulu use loan words abundantly, mainly from English. For example: This situation has led to problems in education because standard Zulu
2880-698: 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 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
2976-538: 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
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3072-422: Is thus still lower in pitch than both of the adjacent syllables. Depressor consonants have an effect called tone displacement . Tone displacement occurs whenever a depressor occurs with a high tone, and causes the tone on the syllable to shift rightward onto the next syllable. If the next syllable is long, it gets a falling tone, otherwise a regular high tone. If the penultimate syllable becomes high (not falling),
3168-718: The Blyde River Canyon , Three Rondavels , and God's Window . It then extends farther north to Hoedspruit in southeastern Limpopo where it 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
3264-541: 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
3360-692: 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 . The escarpment winds north from there, through Mpumalanga, where it includes features such as
3456-584: 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
3552-536: 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 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
3648-475: 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
3744-624: The Northern Ndebele language ( isiNdebele ) is closely related to Zulu. Xhosa , the predominant language in the Eastern Cape , is often considered mutually intelligible with Zulu, as is Northern Ndebele . Maho (2009) lists four dialects: central KwaZulu-Natal Zulu, northern Transvaal Zulu, eastern coastal Qwabe, and western coastal Cele. The Zulu, like Xhosa and other Nguni people , have lived in South Africa for hundreds of years. The Zulu language possesses several click sounds typical of Southern African languages, not found in
3840-645: The Vanderkloof Dam . From the border of Lesotho to below the Vanderkloof Dam, the river bed is deeply incised. Further downstream, the land is flatter, and the river is used extensively for irrigation. At the western point of the Free State, southwest of Kimberley , the Orange meets with its main tributary, the Vaal River , which forms much of the northern border of the province. From here,
3936-528: The sluices of the dams being open, a canoeist (or rafter) can easily travel 30 kilometres (19 mi) per day. The lower reaches of the river are most popular, because of the spectacular topography. Commercial tours are available, and these expeditions depart from the border town of Vioolsdrif . The Orange River has no large animals. It lies outside the range of the Nile crocodile , and although hippopotami were once abundant, they were hunted to extermination in
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4032-687: 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
4128-416: The "teacher" meaning. In principle, every syllable can be pronounced with either a high or a low tone. However, low tone does not behave the same as the other two, as high tones can "spread" into low-toned syllables while the reverse does not occur. A low tone is therefore better described as the absence of any toneme; it is a kind of default tone that is overridden by high or falling tones. The falling tone
4224-493: The 19th century. The Orange River has a relative paucity of species diversity. Surveys from 1995 to 2001 in the Lower Orange River found 19 different fish species from eight different families. The two non-native species recorded in the surveys were Cyprinus carpio and Oreochromis mossambicus , the latter of which had increased rapidly in abundance since the early 1980s. Another exotic species, rainbow trout ,
4320-821: 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
4416-480: 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
4512-510: 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
4608-526: The Gariep Dam and the Vanderkloof Dam. The hydroelectric power station at the Vanderkloof Dam was the first power-generation station in South Africa situated entirely underground. The towns Oviston and Oranjekrag were established to facilitate the construction and operation of the new infrastructure. Irrigation in the vast area downstream of the Vanderkloof Dam, which has turned thousands of hectares of arid veld into highly productive agricultural land,
4704-495: 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 ) 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
4800-534: The Orange River have grown in importance. Irrigation in the Eastern Cape has also received a tremendous boost, not only from the additional water being made available, but also owing to improvement in water quality. Without this improvement, the citrus farmers along the Lower Sundays River would almost certainly have continued to suffer losses of productivity. The Lesotho Highlands Water Project
4896-580: The Orange River inside Lesotho is known as the Senqu . Parts of the Senqu River freeze in winter because of the high altitude. This creates droughts downstream, which mainly affect goat and cattle production. The Orange River then runs westward through South Africa, forming the south-western boundary of the Free State province . In this section, the river flows first into the Gariep Dam and later into
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#17327662989414992-530: The Orange, where the river descends 122 m (400 ft) in a course of 26 km (16 mi). The Orange empties into the Atlantic Ocean between the small towns of Oranjemund (meaning "Orange mouth ") in Namibia and Alexander Bay in South Africa, about equidistant between Walvis Bay and Cape Town . Some 33 km (21 mi) from its mouth, it is obstructed by rapids and sand bars and
5088-477: The Orange. Today, several commercial diamond mines operate along the final stretch of the Orange River and around its mouth. Because of the lack of dangerous animals and high water levels during summer, the river is used for recreational canoeing and rafting . Orange River rafting has become very popular with many companies using their camps along the river from which to operate. The most popular trips are four-day and six-day river trips that take place either along
5184-684: The South African economy by providing water for irrigation and hydroelectric power . The river was named the Orange River in honour of the Dutch ruling family, the House of Orange , by the Dutch explorer Robert Jacob Gordon . Other names include simply the word for river, in Khoekhoegowab orthography written as !Garib , which is rendered in Afrikaans as Gariep River with the intrusion of
5280-666: The Tugela River-Vaal River pumped storage scheme , which used the Sterkfontein Dam , located near Harrismith in the Free State. In 1867, the first diamond discovered in South Africa, the Eureka Diamond , was found near Hopetown on the Orange River. Two years later, a much larger diamond known as the Star of South Africa was found in the same area, causing a diamond rush. This was soon eclipsed by
5376-578: 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
5472-419: 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
5568-413: The color of its tributary, the Vaal River , which name is derived from the name ǀHaiǃarib "pale river" ( vaal being Afrikaans for pale or grey). Since the end of apartheid , the name "Gariep" has had greater favour in official correspondence in South Africa, although the name "Orange" has greater international recognition. In Lesotho, where the river rises, it is known as the Senqu River, derived from
5664-530: 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
5760-405: The diamond rush to mine diamonds directly from kimberlite at Kimberley in 1871, although alluvial diamonds continued to be found in the Orange. Today, several commercial diamond mines operate on the last stretch of the river, as well as the beaches around its mouth. Diamond mines also operate on the middle stretch of the river. During the temperate months of March and April, given good rains and
5856-580: 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
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#17327662989415952-410: 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 the escarpment forms part of the international border between Lesotho and the South African province of KwaZulu-Natal . The escarpment seen from below resembles
6048-710: 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
6144-422: The final syllable dissimilates and becomes low if it was not already. Tone displacement is blocked under the following conditions: Whenever tone displacement is blocked, this results in a depressor syllable with a high tone, which will have the low-tone onset as described above. When the following syllable already has a high or falling tone, the tone disappears from the syllable as if it had been shifted away, but
6240-451: The first full-length feature film in Zulu, Yesterday , was nominated for an Oscar . The mutual intelligibility of many Nguni languages has increased the likelihood of Zulu becoming the lingua franca of the eastern half of the country. In the 1994 film The Lion King , in the " Circle of Life " song, the phrases Ingonyama nengw' enamabala (English: A lion and a leopard spots ), Nans' ingonyama bakithi Baba (English: Here comes
6336-780: The following consonant, although the difference between homorganic nonsyllabic /mC/ and syllabic /m̩C/ is distinctive, e.g. umpetshisi /um̩pétʃiːsi/ "peach tree" (5 syllables) versus impoko /ímpoːɠo/ "grass flower" (3 syllables). Moreover, sequences of syllabic m and homorganic m can occur, e.g. ummbila /úm̩mbíːla/ "maize" (4 syllables). Recent loanwords from languages such as English may violate these constraints, by including additional consonant clusters that are not native to Zulu, such as in igremu /iːgreːmu/ " gram ". There may be some variation between speakers as to whether clusters are broken up by an epenthetic vowel or not, e.g. ikhompiyutha /iːkʰompijuːtʰa/ or ikhompyutha /iːkʰompjuːtʰa/ "computer". Stress in Zulu words
6432-441: The following syllable's tone is not modified. Some examples: Palatalization is a change that affects labial and alveolar consonants whenever they are immediately followed by /j/ . While palatalization occurred historically, it is still productive and occurs as a result of the addition of suffixes beginning with /j/ . A frequent example is the diminutive suffix -yana . Moreover, Zulu does not generally tolerate sequences of
6528-735: The gorge below the Augrabies Falls or along the Richtersveld area. The Orange River Project (ORP) was one of the largest and most imaginative projects of its kind in South Africa. It was constructed by Hendrik Verwoerd 's government at the height of the apartheid era. The ORP was built to exploit the waters of the Orange River—which, without the Vaal River, represents some 14.1% of the total runoff in South Africa—and in
6624-401: 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 the evolution of the mountain landscapes because it helps to shape
6720-420: 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
6816-479: The land area of South Africa (1,221,037 km (471,445 sq mi)). Around 366,000 km (141,000 sq mi) (38%), however, are situated outside the country in Lesotho, Botswana, and Namibia. Some of the earliest precolonial inhabitants called the river ǂNūǃarib , referring to its black colour, or sometimes just Kai !Arib ("Great River"), from which is derived the Afrikaans version Gariep , and translation "Groote Rivier". The early Dutch name for
6912-563: The last 800 km (500 mi) of its course, the Orange receives many intermittent streams (such as the Fish River ), and several large wadis lead into it. In this section, the Namib Desert terminates on the north bank of the river, so under normal circumstances, the volume of water added by these tributaries is negligible. Here, the bed of the river is once again deeply incised. The Augrabies Falls are located on this section of
7008-452: The latter is the class 9 noun prefix in- , which ends in a homorganic nasal. Prenasalisation triggers several changes in the following consonant, some of which are phonemic and others allophonic. The changes can be summed as follows: Zulu has tonic assimilation : high tones tend to spread allophonically to following low-tone syllables, raising their pitch to a level just below that of adjacent high-tone syllables. A toneless syllable between
7104-415: The latter without the h . Nouns are written with their prefixes as one orthographical word. If the prefix ends with a vowel (as most do) and the noun stem also begins with a vowel, a hyphen is inserted in between, e.g. i-Afrika . This occurs only with loanwords. Here are some of the main features of Zulu: The root can be combined with several prefixes and thus create other words. For example, here
7200-578: The majority of South Africa's water, the Orange River plays a major role in supporting agriculture, industry, and mining. To assist in this, two large water schemes have been created, the Orange River Project and the Lesotho Highlands Water Project . Historically, the river played an important role in the South African diamond rush , with the first diamonds in the country being discovered in alluvial deposits on
7296-592: 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
7392-931: 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
7488-476: The original Khoemana name. The Eastern Cape Geographical Names Committee has advertised its intention to consider a name change from the colonial name, for that portion of the river that forms the border between the Eastern Cape and the Free State, with suggestions being IGqili or Senqu . The advertisement placed in the Aliwal Weekblad newspaper states that the "present name is perceived to have
7584-530: The pattern of tones acts more like a template to assign tones to individual syllables, rather than a direct representation of the pronounced tones themselves. Consequently, the relationship between underlying tone patterns and the tones that are pronounced can be quite complex. Underlying high tones tend to surface rightward from the syllables where they are underlyingly present, especially in longer words. The breathy consonant phonemes in Zulu are depressor consonants or depressors for short. Depressor consonants have
7680-607: The population), and it is understood by over 50% of its population. It became one of South Africa's 12 official languages in 1994. According to Ethnologue , it is the second-most widely spoken of the Bantu languages , after Swahili . Like many other Bantu languages, it is written with the Latin alphabet . In South African English , the language is often referred to in its native form, isiZulu . Zulu migrant populations have taken it to adjacent regions, especially Zimbabwe , where
7776-471: The preceding syllable, resulting in a falling tone contour. For example, the English word spoon was borrowed into Zulu as isipunu , phonemically /ísipúnu/ . The second syllable si assimilates to the surrounding high tones, raising its pitch, so that it is pronounced [ísípʼúːnù] sentence-finally. If tone pitch is indicated with numbers, with 1 highest and 9 lowest pitch, then the pitches of each syllable can be denoted as 2-4-3-9. The second syllable
7872-525: The process, to satisfy an increasing demand for water. The main objectives of the project were: The Gariep Dam near Colesberg is the main storage structure within the Orange River. From here, the water is supplied in two directions, westward along the Orange River (via hydroelectric power generators) to the Vanderkloof Dam and southward through the Orange-Fish Tunnel to the Eastern Cape. Eskom operates hydroelectric power stations at both
7968-538: The rainfall is less than 50 mm (2.0 in) per year. The factors that support evaporation, though, tend to increase in a westerly direction. In the wet season (summer), the Orange river becomes a brown coloured torrent. The huge mass of sediment carried constitutes a long-term threat to engineering projects on the river. The total catchment of the Orange River (including the Vaal) extends over 973,000 km (376,000 sq mi), i.e. equivalent to about 77% of
8064-600: 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
8160-439: The regular pattern. Like almost all other Bantu and other African languages , Zulu is tonal . There are three main tonemes : low, high and falling. Zulu is conventionally written without any indication of tone, but tone can be distinctive in Zulu. For example, the words "priest" and "teacher" are both spelt umfundisi , but they are pronounced with different tones: /úm̩fúndisi/ for the "priest" meaning, and /úm̩fundísi/ for
8256-557: The rest of Africa. The Nguni people have coexisted with other Southern tribes like the San and Khoi. Zulu, like most indigenous Southern African languages, was not a written language until the arrival of missionaries from Europe, who documented the language using the Latin script . The first grammar book of the Zulu language was published in Norway in 1850 by the Norwegian missionary Hans Schreuder . The first written document in Zulu
8352-512: The river flows further westward through the arid wilderness of the southern Kalahari region and Namaqualand in the Northern Cape province to meet with Namibia at 20°E longitude. From here, it flows westward for 550 km (340 mi), forming the international border between the province and Namibia's ǁKaras Region . On the border, the river passes the town of Vioolsdrif , the main border post between South Africa and Namibia. In
8448-510: The river was just that translation, Groote Rivier, meaning "Great River". The river was named the Orange River by Colonel Robert Gordon , commander of the United East India Company (VOC) garrison at Cape Town, on a trip to the interior in 1779. Gordon named the river in honor of William V of Orange . A popular but incorrect belief is that the river was named after the supposedly orange color of its water, as opposed to
8544-431: 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
8640-737: Was a Bible translation that appeared in 1883. In 1901, John Dube (1871–1946), a Zulu from Natal, created the Ohlange Institute, the first native educational institution in South Africa. He was also the author of Insila kaShaka , the first novel written in Zulu (1930). Another pioneering Zulu writer was Reginald Dhlomo , author of several historical novels of the 19th-century leaders of the Zulu nation: U-Dingane (1936), U-Shaka (1937), U-Mpande (1938), U-Cetshwayo (1952) and U-Dinizulu (1968). Other notable contributors to Zulu literature include Benedict Wallet Vilakazi and, more recently, Oswald Mbuyiseni Mtshali . The written form of Zulu
8736-912: Was conceived to supplement the water supply in the Vaal River System. Water is delivered to South Africa by means of the delivery tunnel which passes under the Lesotho South Africa border at the Caledon River , and then under the Little Caledon River south of Clarens in the Free State, and discharges into the Ash River about 30 kilometres (19 mi) further to the north. The scheme became viable when water demands in Gauteng reached levels that could no longer be supported economically by alternative schemes such as
8832-622: Was controlled by the Zulu Language Board of KwaZulu-Natal . This board has now been disbanded and superseded by the Pan South African Language Board which promotes the use of all eleven official languages of South Africa. English, Dutch and later Afrikaans had been the only official languages used by all South African governments before 1994. However, in the Kwazulu bantustan , the Zulu language
8928-493: 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
9024-512: Was made possible by the construction of the Gariep and Vanderkloof Dams. Old established irrigation schemes such as those at Buchuberg , Upington , Kakamas , and Vioolsdrif have also benefitted because regulation of the flow is now possible. On the Namibian side of the river, Aussenkehr produces grapes with the help of water from the Orange. In recent years, the wine-producing areas along
9120-519: Was to indicate the implosive /ɓ/ using the special letter ɓ , while the digraph bh would then be simply written as b . Some references may also write h after letters to indicate that they are of the depressor variety, e.g. mh , nh , yh , a practice that is standard in Xhosa orthography. Very early texts, from the early 20th century or before, tend to omit the distinction between plain and aspirated voiceless consonants, writing
9216-596: Was widely used. All education in the country at the high school level was in English or Afrikaans. Since the fall of apartheid in 1994, Zulu has been enjoying a marked revival. Zulu-language television was introduced by the SABC in the early 1980s and it broadcasts news and many shows in Zulu. Zulu radio is very popular and newspapers such as isoLezwe , Ilanga and UmAfrika in the Zulu language are available in Kwazulu-Natal province and Johannesburg . In January 2005
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