84:
1475:(windmill) in the USA. It was perfected in 1883, and soon South Africa (and elsewhere) produced them in large numbers. These windpumps transformed the Great Karoo, making permanent settlement and stock farming (predominantly sheep) possible over large parts of the Karoo for the first time. Like the Karoo Koppie, the multibladed windpump became an iconic feature of the Great Karoo. Sheep farming and the fencing off of the land have meant that antelope numbers have dwindled significantly, and with them, the big carnivores. Leopards still occur in the mountains, but lions now only occur in nature reserves, where they have been recently reintroduced into the Great Karoo.
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1723:
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1291:, moved through Beaufort West. Early one morning, the town was awakened to a sound like that of a strong wind, and suddenly the town was filled with animals. They devoured every sprig of foliage in the town and surrounding countryside. The last of the continuously moving herd left the town 3 days later, to disappear towards the west. The Karoo looked as if a fire had swept through it. During these migrations, the plains and hillsides on every side were thickly covered by one vast mass of springbok, packed like sheep in a fold. As far as the eye could see, the landscape was alive with them.
64:
1170:
and grasses are deciduous, mainly in response to the irregular rainfall. Much of the Nama Karoo biome is used for sheep and goat farming, providing mutton, wool, and pelts for local and international markets, especially since livestock can frequently be provided with a regular supply of water from boreholes. Overgrazing exacerbates the erosion caused by the violent thunderstorms that occur, infrequently, in the summer. It also promotes the replacement of the grasses by shrubs, especially the less edible varieties such as the threethorn (
906:
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1146:, popularly known as Namaqualand daisies, which put on spectacular flower displays covering vast stretches of the landscape in the southern spring-time (August–September) after good rains in the winter. Grasses are uncommon, making most of the biome unsuitable for grazing. The low rainfall, in fact, discourages most forms of agriculture. An exception is the thriving ostrich-farming industry in the KLein Karoo, which is heavily dependent on supplementary feeding with
747:
621:. It covers two-thirds of South Africa and extends in places to 8000 m below the land surface, constituting an immense volume of rocks which was formed, geologically speaking, in a short period of time. Although almost the whole of the Great Karoo is situated on Karoo Supergroup rocks, the geological Karoo rocks extend over a very much larger area, both within South Africa and Lesotho, but also beyond its borders and onto other continents that formed part of
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1150:. The difference between the succulent Karoo biome and the Nama Karoo biome is that the former receives the little rain that falls as cyclonic rainfall in winter, which has less erosive power than the infrequent but violent summer thunderstorms of the Nama Karoo. Frost is also less common in the succulent Karoo biome than in the Nama Karoo biome. The number of mainly succulent plant species is very high for an arid area of this size anywhere in the world.
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1245:, which always seemed to accompany them. These quagga seemed gentle and easy to domesticate. (A pair of quagga was used to draw a horse carriage through London, more for curiosity than for any superiority the quagga might have had over a horse.) They were consequently also easy prey for hunters, who hunted them for sport rather than their meat. By the middle of the 1800s, they were almost extinct, and in 1883, the last one died in an Amsterdam zoo.
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1514:, with the historic Lord Milner Hotel, which is still operational today. The railway reached this point in 1878, before proceeding to Beaufort West at the foot of the Great Escarpment. From there, it reached the top of the African Plateau near Three Sisters along a valley with such a low gradient that passengers were (and still are) hardly aware that they were ascending the Great Escarpment. From there it continued through the Upper Karoo, to
765:. This occurred about 180 million years ago, when huge volumes of lava were extruded over most of Southern Africa and adjoining regions of Gondwana, both on the surface and deep below the surface between the sedimentary strata. Since this massive extrusion of lava, Southern Africa has undergone a prolonged period of erosion, exposing the older, softer rocks, except where they were protected by a cap of dolerite. The genera present include:
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83:
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468:, one of the main targets of this enterprise, is best viewed from the Southern Hemisphere. The Upper Karoo is indeed an ideal site for an astronomical observatory. This is not only because of the clear skies, absence of artificial lights, and high altitude, but also because it is tectonically completely inactive (meaning that there are no fault lines or volcanoes nearby, and no earth tremors or
1451:-speaking peoples, who lived in small family groups and, it is believed, remained largely in their own "territories", killing their own game, and gathering bulbs and roots and drinking from a spring or other water source within their territory. Sometimes these territories were very large and the family group moved from one part to the other. Their only domestic animals were dogs. The
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1265:, or south through the Camdeboo district. These vast herds moved steadily and inexorably across the plains, trampling all before them, including their own kind. Le Vaillant gave the first eyewitness account of such a migration in 1782. He rode through the herd filling the Plains of Camdeboo, seeing neither the beginning nor end of the moving mass.
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upper, sharp edge of the escarpment. (In other parts of the escarpment, hard erosion-resistant geological layers similarly form the upper, abrupt edge.) Note the island remnants of the earlier extent of the plateau on the plain below the escarpment (the Lower Karoo), left behind as the escarpment has gradually eroded further inland.
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The First World War brought about a slump in the ostrich feather market, but the industry recovered in later years, when not only the feathers were sought after, but also ostrich leather, and its meat, which is very tasty, and a major export item. Today, several farms can be visited by tourists, near
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district was apparently the first person to demonstrate that the ostrich could successfully be domesticated, bred in captivity, and the eggs hatched in incubators, while still producing the magnificent feathers. This idea was quickly adopted by farmers in the Little Karoo, where they started growing
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to the south and the savannah biome to the north. It is defined primarily by the dominance of dwarf (less than 1 m high) shrubs with a co-dominance of grasses especially towards the north-east and east where it grades into the grassland biome of the highveld and the
Eastern Midlands. The shrubs
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The Nama Karoo biome is located entirely on the central plateau mostly at altitudes between 1000 and 1500 m. It incorporates nearly the whole of the historical and geographical Great Karoo, but also includes a portion of southern
Namibia's Namaqualand, and South Africa's Bushmanland (both local
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The lava outpourings that ended the Karoo deposition of rocks, not only covered the
African surface, and other parts of Gondwana with a 1.6 km thick layer basaltic lava, but it also forced its way, under high pressure, between the horizontal layers of sedimentary rocks belonging to the Ecca and
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The Great Karoo straddles the 30° S parallel on the west of the continent, in a similar position to other semidesert areas on earth, north and south of the equator. It is furthermore in the rainfall shadow of the Cape Fold
Mountains along the western coastline. The western "Lower Karoo" (the Tankwa
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The mountain zebra occurred in the mountain regions of the Cape Fold Belt and along the southern portion of the Great
Escarpment. Thus, they were endemic to, amongst others, the western Lower Karoo and the Klein Karoo. However, they were hunted to near extinction, leaving fewer than 100 individuals
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The introduction of the windpump to tap the Great Karoo's underground water resources in the late 1800s made permanent human habitation and sheep farming possible over large parts of the Great Karoo for the first time. As a result, the teeming number of large antelope in the Karoo has dwindled into
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The Klein Karoo contains two other geological features that give the landscape a special character. During the erosion of the
African interior following the bulging of the continent during the massive lava outpourings that ended the Karoo sedimentation 180 million years ago, some of the eroded
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from the air. From about 150 million years ago the South
African surface has been subjected to an almost uninterrupted period of erosion, particularly during the past 20 million years, shaving off many kilometers of sediments. This exposed the dolerite sills, which were more resistant to
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The Klein Karoo's boundaries are sharply defined by mountain ranges to the west, north, and south. The road between
Uniondale and Willowmore is considered, by convention, to form the approximate arbitrary eastern extremity of the Klein Karoo. Its extent is much smaller than that of the Great Karoo.
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A stylized illustration of the Great
Escarpment, based particularly on its appearance in the Great Karoo, where thick erosion resistant dolerite sills (see below; represented here by the thick black lines. The thinner dolerite sills are not drawn in this diagram to avoid clutter) generally form the
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The Klein Karoo, and especially
Oudtshoorn, became synonymous with the ostrich-feather industry in the 1880s. The resulting "feather millionaires" built Victorian "Feather Palaces" all over town, using the red rocks belonging to the Enon Conglomerate, and related Kirkwood Formation, to build them.
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The ostrich is found throughout Africa, but the most handsome specimens came from the Klein Karoo, where the dry weather, but plentiful water in the streams formed an ideal habitat for these large, flightless birds. Here, they grow to over 2 m in height, and weigh over 100 kg. The male's
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During these migrations, the springbok never ran or trotted. On the whole, they were silent, except for the shudder of their stamping hoofs. Nothing could divert them, and hunters could ride amongst them, shooting them at random, without apparently causing alarm. People could move amongst them and
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The second special geological feature that marks the Kelin Karoo is the 300 km-long fault line along the southern edge of the Swartberg Mountains. The Swartberg Mountains were lifted up along this fault, to such an extent that in the Oudtshoorn region, the rocks that form the base of the Cape
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The geology of the Klein Karoo bears no resemblance to that of the Great Karoo (see the diagram on the left, of a NS geological cross-section through the Klein and Great Karoos). The valley is an integral part of the Cape Fold Mountain Belt, with the two ranges on either side composed of extremely
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The Karoo Supergroup was formed in a vast inland basin starting 320 million years ago, at a time when that part of Gondwana which would eventually become Africa, lay over the South Pole. Icebergs that had calved off the glaciers and ice sheets to the north deposited a 1 km-thick layer of
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and the Highveld. The boundary to the east grades into the grasslands of the Eastern Midlands. The Great Karoo is itself divided by the Great Escarpment into the Upper Karoo (generally above 1200–1500 m) and the Lower Karoo on the plains below at 700–800 m. A great many local names, each
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unanimously denounced it as a frightening place of great heat, great frosts, great floods, and great droughts. Today, it is still a place of great heat and frosts, and an annual rainfall of between 50 and 250 mm, though on some of the mountains it can be 250 to 500 mm higher than on the
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and the Seweweekspoort defiles, were subject to periodic flooding, after heavy thunderstorms in the Great Karoo. The Swartberg Pass is not tarred and can be treacherously slippery after rain. It also becomes impassable after heavy snowfalls on the mountain, a not infrequent occurrence in winter.
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of the mid-1700s, who led a nomadic existence, enduring great hardships in the relentless aridity, the intense heat (such that even their dogs could not walk on the scorching ground and had to be lifted into the overcrowded wagons), and the bitter cold in winter, especially at night. Before that
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Probably the strangest and most puzzling zoological phenomenon in the Great Karoo was the periodic, unpredictable appearance of massive springbok migrations. These migrations always came from the north, and could either go west towards Namaqualand and the sea, south-west through towns such as
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The first European settlers landed in the Cape of Good Hope in 1652, and between 1659 and 1664, made several unsuccessful attempts to penetrate the Great Karoo from the south-west. The Europeans who first entered the Great Karoo did so from the south-east (traveling north from
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Karoo and Moordenaarskaroo) contain remnants of the Cape Fold Mountains (e.g. the Witteberg and Anysberg Mountains) which give it a moderate hilly appearance, but further east, the Lower Karoo becomes a monotonously flat plain. The "Upper Karoo" has been intruded by
693:, the lowermost layer of the Karoo Supergroup. As Gondwana drifted northwards, the basin turned into an inland sea with extensive swampy deltas along its northern shores. The peat in these swamps eventually turned into large deposits of coal which are mined in
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range to the south. The northern strip of the valley, within 10–20 km from the foot of the Swartberg mountains is least karoo-like, in that it is a well-watered area both from the rain and the many streams that cascade down the mountain, or through narrow
1365:(20–90 kg) do occur, especially in the mountains, but are very secretive, so are rarely seen. Many of the animals that formerly inhabited the Karoo in large numbers, including lions, have been reintroduced to the area in nature reserves and game farms.
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The Klein Karoo can only be accessed by road through the narrow defiles cut through the surrounding Cape Fold Mountains by ancient, but still flowing, rivers. A few roads traverse the mountains over passes, the most famous and impressive of which is the
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and many others in the Western Cape. The main motivation for building the pass was to provide an all-weather road connection between the southern Great Karoo, and Oudtshoorn (and from there to the sea). The two alternative roads, through the
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Sunset in the Great Karoo, near Sutherland, showing a multibladed windpump, which has made permanent settlement and farming possible in this thirsty land. These windpumps are as iconic of the Great Karoo as are the flat-topped Karoo
2520:
Weishampel, David B; et al (2004). "Dinosaur distribution (Early Jurassic, Africa)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 535–536.
736:, the remnants of which are found only in the immediate vicinity of Lesotho. Several dinosaur nests, containing eggs, some with dinosaur fetal skeletons in them, have been found in these rocks, near what had once been a swampy pan.
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No one knew how, why, or where these migrations started, nor where they ended, nor did anyone know if these animals ever returned to where they had started. The migrations were always unidirectional, from north of the Great Karoo.
600:
A schematic geological map of the outcrops (surface exposures) of the Karoo Supergroup rocks in Southern Africa: The location and approximate structure of the Cape Fold Mountains are also diagrammatically indicated for reference
966:
belonging to the 450- to 510-million-year-old Table Mountain Group (i.e. the oldest layer of the Cape Supergroup). The valley floor is covered, in the main, by the next (younger) layer of the Supergroup, namely the much softer
1341:. Its numbers have been consistently lowering due to destruction of its habitat. They are unique relative to similar species through how they are polygamous and how each female can only produce one or two offspring per year.
224:
and climate, and above all, its low rainfall, arid air, cloudless skies, and extremes of heat and cold. The Karoo also hosted a well-preserved ecosystem hundreds of million years ago which is now represented by many fossils.
284:, which receives only 75 mm of rain annually. The eastern and north-eastern Karoo are often covered by large patches of grassland. The typical Karoo vegetation used to support large game, sometimes in vast herds.
552:
The southern 30– to 50 km-wide strip, north of the Langeberg range, is as arid as the western Lower Karoo, except in the east, where the Langeberg range (arbitrarily) starts to be called the Outeniqua Mountains.
925:. The colour code for the Karoo rocks is the same as those used in the above diagram. The heavy black line flanked by opposing arrows is the fault that runs for nearly 300 km along the southern edge of the
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by the 1930s. Conservation efforts since then brought their numbers up to 1200 by 1998, mainly by concentrating these zebra in nature reserves and protected areas, the most well-known of these being the
1389:), which lives on the plains. The two species are, therefore, rarely seen in the same habitat. The quagga is closely related to Burchell's zebra, and appears also to have been confined to the plains.
1510:, where it followed a course almost midway between the Swartberg Mountains to the south and the Great Escarpment to the north. Along the way, it passed through the quaint Victorian village of
327:, looking south across the plains of the Lower Karoo: Note the remnants of the former extent of the central plateau on the plain below the escarpment (see diagram on the right). Also note the
1073:, are more extensive than the geographical or historical Karoo described in South African atlases and guide books (compare the map on the right with the map at the beginning of the article).
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1619:
This area was explored by European settlers in the late 17th century, who encountered the Khoisan people as the original inhabitants of this area. The latter called the Swartberg Mountains
63:
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tusks have been found by farmers in the Camdeboo district, but no records exist of any having been seen alive in that region. The quagga roamed the Karoo in great numbers together with
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activity took place on a titanic scale, which brought an end to a flourishing reptile evolution. These genera represent some of the extinct, mainly predinosaur, animals of the Karoo:
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on the other side of the Swartberg mountains in the Great Karoo. Also, the main road between Oudtshoorn and George, on the coastal plain, crosses the mountains to the south via the
480:
The Klein Karoo is separated from the Great Karoo by the Swartberg Mountain range. Geographically, it is a 290 km-long valley, only 40–60 km wide, formed by two parallel
1611:
have been established in many parts of the Great Karoo, turning what was once regarded as a forbiddingly desolate and unattractive geographical barrier into a tourist destination.
444:
Highveld do at times experience lower temperatures than Sutherland, but not as consistently as Sutherland does. Snowfalls are not infrequent during the southern winter months. The
365:. The Hantam, Kareeberge, Roggeveld, and uweveldare the better known subregions of the Upper Karoo, though most of it is simply known as the Upper Karoo, especially in the north.
1333:, a critically endangered animal, lives exclusively in seasonal river basins and a very particular set of scrubland in the central semiarid region in the Karoo. It is hunted by
1001:", as they are known, were deposited by high energy, fast flowing rivers, and are found between Calitzdorp and Oudtshoorn, where they form the strikingly red "Redstone Hills".
1888:
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of South Africa. No exact definition of what constitutes the Karoo is available, so its extent is also not precisely defined. The Karoo is partly defined by its topography,
440:, at 1456 m above sea level, which is reputedly the coldest town in South Africa with average minimum temperatures of −6.1 °C during winter. Parts of the eastern
357:
denoting different subregions of the Great Karoo, exist, some more widely, or more generally, known than others. In the Lower Karoo, going from west to east, they are the
732:
After the Beaufort period, Southern Africa (still part of Gondwana) became an arid sand desert with only ephemeral rivers and pans. These sands consolidated to form the
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struggle over the Karoo's vast expanses, it was a bloody war of attrition wherein both sides used newly developed technologies to their advantage. Numerous abandoned
228:
The ǃ’Aukarob formed an almost impenetrable barrier to the interior from Cape Town, and the early adventurers, explorers, hunters, and travelers on the way to the
950:
erosion than the Karoo sediments, forming one of the most characteristic features of the Karoo landscape, namely the flat topped hills, called "Karoo Koppies".
609:
refers to an extensive and geologically recent (180–310 million years old) sequence of sedimentary and igneous rocks, which is flanked to the south by the
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and Moordenaarskaroo regions of the Lower Karoo, and adjoining Upper Karoo region of the geographic Great Karoo. It also occurs to the south, in part of the
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plains. However, underground water is found throughout the Karoo, which can be tapped by boreholes, making permanent settlements and sheep farming possible.
1455:-speaking agriculturalists to the east of the Great Karoo did not occupy this arid region due to the scarce rainfall which prevented the farming of cattle.
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1596:
can still be seen at strategic locations, especially along the railway line, throughout the Great Karoo. A prime example still "guards" a bridge over the
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kill them with sticks, or cripple them by seizing a leg and breaking it. Not only people followed these herds for the easy meat they provided, but also
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1414:
lucerne as the birds' favorite food. During 1880, no less than 74,000 kg of feathers were exported, and in 1904, it passed the 210,000-kg mark.
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As in the Great Karoo, antelope and other big game inhabited the Klein Karoo in the past. However, the dominant zebra was not the quagga, but the
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348:
to the south and south-west. The extent of the Karoo to the north is vague, fading gradually and almost imperceptibly into the increasingly arid
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magisterial district, in particular, contributing a significant number of fighters to the Republican cause. Fought both conventionally and as a
761:. This is solidified lava that was forced under high pressure between the horizontal strata of the sedimentary rocks that make up most of the
3141:
2311:
1119:. None of these regions is ever referred to, either geographically or locally, as "Karoo". However, it has a major extension inland into the
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Mountains. The Swartberg range owes some of its great height to upliftment along this fault line. The subsurface structures are not to scale.
460:
which will, 2500 in total, be scattered in other parts of South Africa and Australia, to survey the southern skies at radio frequencies. Our
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1638:, from where the ostrich feathers from the Klein Karoo's ostrich farms could be exported to Europe. That line is no longer in use today.
1165:
geographical names, not names of biomes). It is the second-largest biome in South Africa, and forms the botanical transition between the
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sills which top the escarpment and mountains in the middle distance, giving these structures their characteristic flat-topped appearance.
96:
which delimits the Central South African Plateau. To the immediate south and south-west the solid lines trace the parallel ranges of the
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A diagrammatic 400 km north–south cross-section through the southern portion of the country at approximately 21° 30' E (i.e. near
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has an emplacement of telescopes about 20 km east of the town, on a small plateau 1798 m above sea level, and is home to the
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has classified the Great Karoo and Klein Karoo as almost entirely within two of what they consider South Africa's eight botanical
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in the Great Karoo. Cape mountain zebras are still found in protected areas managed by Cape Nature, including the Kamanassie and
705:, laid down on a vast plain with Mississippi-like rivers depositing mud from an immense range of mountains to the south. Ancient
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in the Swartberg from the Great Karoo. The main towns of the region are situated along this northern strip of the Klein Karoo:
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feathers have been prized by many cultures in Africa, Europe, and Asia over thousands of years. In the 1860s, a farmer in the
569:. The only exit from the Klein Karoo that does not involve crossing a mountain range is through the 150 km-long, narrow
452:, the largest optical telescope in the Southern Hemisphere. To the north, still on the Plateau, and 75 km north-west of
287:
Today, sheep thrive on the xerophytes, though each sheep requires about 4 hectares (9.9 acres) of grazing to sustain itself.
1526:, was found. The Orange River, at this point, forms the local unofficial boundary between the Great Karoo and the Highveld.
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1221:, the famous French explorer, naturalist, and ornithologist, who traveled through the Great Karoo in the 1780s, killed a
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shales. The dolerite of the Great Karoo did not penetrate these rocks, so Karoo Koppies are not seen in the Klein Karoo.
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1381:) which is adapted for life on rugged, mountainous terrain. Their hooves are harder and faster-growing than those of
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1486:, in the Lower Karoo, next to the Matjiesfontein railway station, on the railway line from Cape Town to Johannesburg
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Flat-topped hills (called Karoo Koppies) are highly characteristic of the southern and southwestern Karoo landscape.
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in the Great Fish River in the Karoo (and ate its foot for breakfast). He also recorded that he saw the spoor of a
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Great locust swarms also frequently invaded or arose in the Great Karoo, and still occur from time to time today.
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through a hub at De Aar, in the Great Karoo. Further branch lines were later built from points further north to
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The Karoo is divided into the Great Karoo and the Klein Karoo. The Klein Karoo is delimited in the south by the
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A railway line was built to connect Calitzdorp and Oudtshoorn, to Willowmore and from there, via Klipplaat, to
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McCarthy, T.S. (2013) The Okavango delta and its place in the geomorphological evolution of Southern Africa.
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The vegetation of the Upper is similar to the Lower Karoo, so few people make a distinction between the two.
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Supergroup are exposed. These are locally known as the Cango Group, but are probably continuous with the
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403:(see below), creating multiple flat-topped hills, or Karoo Koppies, which are iconic of the Great Karoo.
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421:. Thereafter, they gradually ascend the Great Escarpment along a broad valley to Three Sisters on the
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The main highway (the N1) and railway line from Cape Town to the north enter the Lower Karoo from the
92:, with the names of surrounding areas in blue. The thick interrupted line indicates the course of the
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The succulent Karoo biome is dominated by dwarf, leafy-succulent shrubs, and annuals, predominantly
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towards the north-west. To the north and north-east, it fades into the savannah and grasslands of
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1361:(3.0–6.2 kg) are arguably the largest predators likely to be seen in the Great Karoo today.
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The only sharp and definite boundary of the Great Karoo is formed by the most inland ranges of
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1965:. (5th Ed. 1993). pp. 78–89. Reader’s Digest Association of South Africa Pty. Ltd., Cape Town.
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8:
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4004:
3920:
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1774:
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insignificance, and with them, the large carnivores have all but disappeared. Today, the
1338:
1253:
1124:
1054:
946:
914:
618:
493:
433:
345:
320:
296:
2364:
Bulpin, Thomas Victor (1985). "7. The lost world of the dinosaurs: The Karoo sequence".
4884:
4781:
4702:
4562:
4512:
4351:
4222:
4185:
4160:
4150:
4145:
4130:
4120:
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2799:
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2602:
2144:
2001:
1976:
1646:
1178:
718:
526:
498:
414:
2966:. (7th Edition). p. 531, 497. Trustees of the John Voelcker Bird Book Fund, Cape Town.
1677:, in his 1901 poem "Bridge-Guard in the Karroo", evoked the loneliness experienced by
1631:
These grand red palaces and other buildings in Oudtshoorn can still be admired today.
975:
material was trapped in the valleys of the Cape Fold Mountains, especially during the
544:
Farmlands along the well-watered, fertile foothills of the more than 2000 m-high
4919:
4879:
4823:
4709:
4432:
4252:
4212:
3766:
3231:
3206:
3196:
3017:
2815:
2771:
2755:
2706:
2522:
2437:
2394:
2369:
2160:
2006:
1589:
1088:
422:
89:
2900:
2729:
2489:
4924:
4814:
4714:
4527:
4399:
4284:
4202:
4135:
3050:
3036:. Northumberland Avenue, London. 1898. p. 26. "The Railway System of South Africa".
2997:
2918:
2432:
Walton, Christopher, ed. (1984). "Anatomy of South Africa: 200 million years ago".
1996:
1988:
1166:
1070:
918:
762:
713:
prospered in the wet forests, and their remains have made the Karoo famous amongst
682:
634:
606:
591:
410:
272:. The driest region of the Karoo, however, is its southwestern corner, between the
245:
221:
159:
2225:
p. 89-90, 102–107, 134–136,159–161, 195–211, 248–254. Struik Publishers, Cape Town
1283:
In 1849, a massive herd of springbok, amongst which were intermingled wildebeest,
264:, spaced 50 cm or more apart, and becoming very sparse going northwards into
4818:
4495:
4288:
4195:
4097:
3246:
2735:
2661:
2630:
2608:
2564:
2339:
1892:
1853:
1686:
1674:
1573:
1468:
1452:
1330:
1128:
1103:
geographical region, about 250 km north of Cape Town, and continues through
1100:
1082:
1062:
1046:
968:
905:
714:
614:
574:
353:
269:
261:
30:
This article is about the semidesert region of South Africa. For other uses, see
3065:
2988:
Moodley, Y. & Harley, E.H. (2006) Population structuring in mountain zebra (
2389:
Reid, R., ed. (2005). "7. The lost world of the dinosaurs: The Karoo sequence".
2354:(1975); Macropaedia, Vol. 17. p. 60. Helen Hemingway Benton Publishers, Chicago.
4958:
4805:
4557:
4552:
4517:
4437:
4379:
4240:
3942:
3241:
1635:
1546:
1523:
1511:
1483:
1478:
1131:. From here, it continues eastwards into the western half of the Klein Karoo.
1014:
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942:
938:
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878:
807:
795:
783:
758:
722:
610:
566:
558:
481:
429:
400:
217:
198:
97:
69:
3001:
2458:
2308:"273 Precision Actuators for the Largest Telescope in the Southern Hemisphere"
941:. The long vertical fissures through which the lava welled up solidified into
596:
4952:
4894:
4860:
4855:
4522:
4485:
4314:
4261:
3952:
3881:
3876:
3103:
2909:
2068:. Micropaedia, Vol. 6. (2007). p. 750. Encyclopædia Britannica Inc., Chicago.
1804:
1729:
1702:
1671:
wrote of the Karoo in his 1899 poem "Drummer Hodge" (or "The Dead Drummer").
1458:
1448:
1410:
1358:
1308:
1262:
1189:
1184:
894:
694:
418:
324:
124:
111:
2271:. pp. 271–274, 301–314. Discovering Southern Africa Productions, Muizenberg.
4832:
4827:
4801:
4661:
4500:
4337:
4256:
4245:
4230:
4155:
3891:
3886:
3871:
3866:
3226:
3150:
3046:
2010:
1992:
1668:
1641:
The Swartberg Pass was built, with convict labor, between 1881 and 1888 by
1564:
1558:
1550:
1288:
1222:
1134:
1112:
1108:
1092:
1018:
840:
726:
530:
303:
that also runs east–west. The Great Karoo lies to the north the Swartberg.
144:
3099:
4810:
4796:
4590:
4542:
4537:
4478:
4468:
4280:
4270:
3947:
3896:
3861:
3577:
3221:
3201:
1682:
1624:
1581:
1491:
1104:
1026:
1025:, into which an underground stream has carved the impressively extensive
872:
855:
802:
778:
746:
534:
469:
417:
and follow a course about 50 km south of the Great Escarpment up to
3119:
2541:
Van Deventer, L. & McLennan, B. (eds) (2010). "The Little Karoo" in
1842:. (1984). p. 13, 98–106, 114–119. Reader’s Digest Association, Cape Town
717:. The first of these Karoo fossils was discovered in 1838 by Scots-born
4865:
4845:
4840:
4595:
4345:
4323:
4298:
4293:
3925:
3913:
1678:
1593:
1444:
1334:
1238:
1226:
1159:
1143:
1066:
976:
910:
867:
770:
518:
514:
441:
335:
3114:
2624:
2129:. p. 206-223, 243–247, 252–273, 300–311. Struik Publishers, Cape Town.
1436:), which is slightly less arid than the western Karoo. These were the
311:
4874:
4870:
4750:
4567:
4389:
4369:
4332:
4328:
4046:
3937:
3261:
3083:
1608:
1438:
1433:
1273:
1210:
1022:
981:
963:
960:
926:
849:
814:
710:
570:
545:
510:
506:
489:
485:
465:
379:
300:
277:
253:
237:
2195:. (1970). Council for Geoscience, Geological Survey of South Africa.
1529:
The line reached Kimberley in 1885, and has since been extended via
1217:, and other large game, especially on the grassy flats in the east.
988:
428:
Turning north from the N1 between Touws River and Beaufort West, at
88:
Extent of the Karoo (olive-green) and Klein Karoo (bright green) in
4836:
4341:
4015:
3908:
3216:
1585:
1577:
1534:
1530:
1519:
1472:
1362:
1277:
1234:
1206:
935:
887:
883:
860:
845:
828:
822:
790:
755:
740:
729:
recognised the Karoo fossils' mammal-like characteristics in 1897.
721:
at a road cutting near Fort Beaufort. He sent his specimens to the
622:
397:
328:
257:
249:
229:
202:
195:
1037:
299:
that run east–west parallel to the coast, and in the north by the
4850:
4505:
4374:
4318:
4302:
4235:
3903:
1542:
1346:
1304:
1300:
1284:
1242:
1147:
1116:
1096:
1045:, or botanical regions, of South Africa bear the name Karoo: the
833:
819:
706:
690:
665:
649:
522:
2436:. The Reader's Digest Association South Africa. pp. 14–15.
2282:"Deep Space Observatories: The Southern African Large Telescope"
1604:, in the Lower Karoo, between Matjiesfontein and Beaufort West.
697:
and on the Highveld. This 3 km-thick layer is known as the
1554:
1538:
1515:
1316:
1214:
548:(in the background) along the northern strip of the Klein Karoo
461:
214:
174:
3109:
1685:
while guarding the Karoo railway track, a lifeline during the
1627:
in the Swartberg Mountains are named after this Khoisan word.
685:
of varying origins and sizes into this basin. This became the
613:, and to the north by the more ancient Ventersdorp Lavas, the
540:
2898:
1977:"Recovery from the most profound mass extinction of all time"
1312:
1115:, and on into the Namaqualand or Namaland region of southern
1058:
1042:
628:
1296:
241:
210:
177:
165:
2417:. p. 6-7. Keyworth, Nottingham: British Geological Survey.
1580:
units, reinforced by the sympathizers ("rebels") from the
1049:
to the west of green line, and the Nama Karoo to the east.
913:
in the Klein Karoo), showing the relationship between the
754:
Karoo Koppies hills are capped by hard, erosion-resistant
2514:
1248:
2084:. (5th Ed.) pp. 106–117. Conolly Publishers, Scottburgh.
2056:. p. 12-13, 120, 126, 140–146. Fontana/ Collins, London.
1276:, one of Southern Africa's most well-known antelopes or
2310:. Physik Instrumente (PI) GmbH & Co. KG. May 2003.
1981:
Proceedings of the Royal Society B: Biological Sciences
2962:
Hockey, P.A.R., Dean, W.R.J. & Ryan, P.G. (2005).
1974:
1600:, 12 km (7.5 mi) to the east of the town of
525:, as well as such well-known mission stations such as
361:, the Moordenaarskaroo, the Koup, the Vlakte, and the
2992:):the molecular consequences of divergent histories.
2193:
Geological Map of South Africa, Lesotho and Swaziland
186:
162:
1963:
Reader’s Digest Illustrated Guide to Southern Africa
1256:'s menagerie at Versailles by Nicolas Marechal, 1793
432:, the road ascends the Great Escarpment through the
171:
1205:The Great Karoo used to support a large variety of
168:
1852:
1490:In 1872, construction was started to connect the
1021:. In the Klein Karoo, the outcrop is composed of
4950:
2188:
2186:
2184:
2182:
2180:
2178:
2176:
1447:-speaking clans migrating through the area, and
1418:Oudtshoorn, the center of the ostrich industry.
2977:Raptor Identification Guide for Southern Africa
1968:
1851:
1918:Potgieter, D.J. & du Plessis, T.C. (1972)
573:valley between Uniondale and Humansdorp, near
4766:
4626:Geographic data and information organizations
4031:
3135:
2924:10.2305/IUCN.UK.2019-1.RLTS.T3326A45176532.en
2575:
2573:
2173:
1095:northwards to over 200 km into southern
953:
701:, which is overlain by the 5.6 km-thick
3045:
2678:
2676:
2674:
2672:
2670:
2594:
2592:
2590:
2588:
194:; from the Afrikaans borrowing of the South
3034:Proceedings of the Royal Colonial Institute
2979:. pp. 62, 82. Rollerbird Press, Pinegowrie.
2217:
2215:
2213:
2211:
2209:
2207:
2205:
2203:
2201:
1099:. It starts in the south just north of the
4773:
4759:
4038:
4024:
3142:
3128:
3016:. Cape Town. Human & Rousseau, p. 95.
2945:
2943:
2941:
2899:Collins, K.; Bragg, C.; Birss, C. (2019).
2870:"Bunolagus monticularis (Riverine rabbit)"
2582:. (1999) p. 90. Times Books Group, London.
2580:The Times Comprehensive Atlas of the World
2570:
2427:
2425:
2423:
2263:
2261:
2259:
2257:
2255:
2253:
2251:
1958:
1956:
1954:
1952:
1950:
1948:
1914:
1912:
1910:
1908:
1906:
1904:
1902:
1900:
1522:, where South Africa's first diamond, the
629:Geological history of the Karoo Supergroup
561:between Oudtshoorn in the Klein Karoo and
4677:National Council for Geographic Education
3149:
2951:Field Guide to Mammals of Southern Africa
2922:
2667:
2585:
2545:. p. 58-61. Struik Publishers, Cape Town.
2459:"Early dinosaurs crawled before they ran"
2249:
2247:
2245:
2243:
2241:
2239:
2237:
2235:
2233:
2231:
2132:
2121:
2119:
2117:
2115:
2113:
2111:
2109:
2107:
2105:
2087:
2076:
2074:
2059:
2048:
2046:
2044:
2042:
2040:
2000:
1946:
1944:
1942:
1940:
1938:
1936:
1934:
1932:
1930:
1928:
1920:Standard Encyclopaedia of Southern Africa
1087:The succulent Karoo biome runs along the
917:(and their geological structure) and the
68:Typical Karoo vegetation to the south of
2975:Oberprieler, U. & Cillié, B. (2002)
2837:"Bunolagus monticularis riverine rabbit"
2198:
2038:
2036:
2034:
2032:
2030:
2028:
2026:
2024:
2022:
2020:
1922:. Vol. 6. pp. 306–307. Nasou, Cape Town.
1563:
1506:and entered the Lower Karoo through the
1477:
1457:
1267:
1247:
1133:
1076:
1036:
904:
745:
595:
539:
334:
310:
2956:
2938:
2647:
2645:
2643:
2641:
2639:
2537:
2535:
2450:
2420:
2393:. Struik Publishers. pp. 199–221.
1897:
1835:
1833:
1831:
1829:
1827:
1825:
1823:
1821:
1819:
1192:plant species in the Nama Karoo biome.
580:
14:
4951:
4780:
3063:
2982:
2820:: CS1 maint: archived copy as title (
2776:: CS1 maint: archived copy as title (
2711:: CS1 maint: archived copy as title (
2543:South Africa by Road, a Regional Guide
2502:from the original on 28 September 2007
2481:
2456:
2431:
2363:
2228:
2165:: CS1 maint: archived copy as title (
2102:
2071:
1925:
1662:
739:Finally, about 180 million years ago,
456:, seven radio dishes form part of the
446:South African Astronomical Observatory
4754:
4019:
3123:
3066:""Bridge-Guard in the Karroo": Notes"
2864:
2862:
2847:from the original on 14 December 2014
2487:
2368:. Books of Africa. pp. 199–221.
2314:from the original on 29 February 2012
2017:
1623:meaning "a place rich in water". The
1069:, although both, like the geological
4931:
4721:
4045:
3852:South African Bantu-speaking peoples
2636:
2532:
2388:
1873:participating institution membership
1816:
1443:time, the only inhabitants were the
919:geology of the Klein and Great Karoo
278:Cederberg-Skurweberg mountain ranges
4733:
2953:p. 136, 170, 176. Struik, Cape Town
2949:Stuart, C. & Stuart, T (2007).
2910:IUCN Red List of Threatened Species
2221:McCarthy, T., Rubridge, B. (2005).
1800:Central Karoo District Municipality
1681:soldiers at Ketting station on the
1494:'s coastal railway system with the
1153:
1041:Two separate and independent Karoo
76:Mountains visible in the background
24:
2859:
2469:from the original on 17 April 2009
2082:Conolly’s Guide to Southern Africa
1518:, and crossed the Orange River at
1188:). However, there are few rare or
934:Beaufort groups, to solidify into
585:
27:Semi-desert region in South Africa
25:
4995:
3092:
2880:from the original on 28 June 2015
2413:Jackson, A.A., Stone, P. (2008).
2366:Scenic Wonders of Southern Africa
2288:from the original on 4 March 2012
2125:Norman, N., Whitfield, G. (2006)
1975:Sahney, S.; Benton, M.J. (2008).
1568:A blockhouse in the eastern Karoo
1421:
1252:Painting of a quagga stallion in
921:, as well as the position of the
488:to the north, and the continuous
472:occur, even at great distances).
4930:
4918:
4907:
4906:
4893:
4732:
4720:
4708:
4697:
4696:
4672:International Geography Olympiad
3098:
3082:The poem was first published in
3072:from the original on 28 May 2012
2964:Roberts Birds of Southern Africa
2096:South African Journal of Geology
1751:
1736:
1721:
1709:
1694:
1614:
1426:
1368:
1200:
1061:, they have coined their biomes
664:
648:
475:
450:Southern African Large Telescope
390:
158:
82:
62:
4969:Natural regions of South Africa
3057:
3039:
3026:
3006:
2969:
2892:
2829:
2785:
2741:
2720:
2614:
2548:
2407:
2382:
2357:
2345:
2326:
2300:
2274:
2066:The New Encyclopædia Britannica
1576:of 1899–1902, three Republican
4385:Geographic information science
1879:
1845:
1758:Farmhouse in the Tankwa Karoo.
1728:The Valley of Desolation near
1607:Recently, nature reserves and
1195:
1032:
1017:, and similar outcrops in the
368:
306:
39:Natural region in South Africa
13:
1:
4491:Geographic information system
2457:Knight, Will (28 July 2005).
2391:The Story of Earth & Life
2223:The Story of Earth and Life.
1810:
1533:(then Bechuanaland) to reach
1138:Spring flowers in Namaqualand
890:herbivorous, bipedal dinosaur
297:Outeniqua–Langeberg Mountains
4418:Environmental social science
3106:travel guide from Wikivoyage
1780:Mountain Zebra National Park
1701:The Nuweveld Mountains near
1395:Mountain Zebra National Park
385:
290:
7:
3110:http://www.karoospace.co.za
2269:Discovering Southern Africa
1795:Karoo District Municipality
1763:
1743:Typical Karoo koppies near
1111:, immediately south of the
315:A view from the top of the
10:
5000:
3014:Early Railways at the Cape
1790:Tankwa Karoo National Park
1502:, The new line started in
1357:(3.0–5.8 kg) and the
1157:
1080:
954:Geology of the Klein Karoo
632:
589:
268:and, from there, into the
29:
4964:Geography of South Africa
4902:
4891:
4788:
4692:
4649:
4618:
4581:
4533:Global Positioning System
4459:
4450:
4408:
4360:
4221:
4096:
4089:
4056:
3977:
3842:
3752:
3629:
3620:
3515:
3506:
3417:
3408:
3314:
3305:
3280:
3170:
3161:
3002:10.1007/s10592-005-9083-8
1860:Oxford English Dictionary
1482:The Lord Milner Hotel in
1471:invented the multibladed
1403:Gamkaberg Nature Reserves
959:hard, erosion-resistant,
774:, aquatic Dwyka carnivore
642:Extinct Karoo vertebrates
605:In geological terms, the
140:
105:
81:
61:
54:
44:
3032:Royal Colonial Society:
2633:. Accessed 30 April 2014
2434:Atlas of Southern Africa
2415:Bedrock Geology UK South
1840:Atlas of Southern Africa
725:, where fellow Scotsman
689:consisting primarily of
301:Swartberg Mountain Range
4979:Physiographic provinces
4641:National mapping agency
4606:Survey (human research)
4548:Participant observation
3573:State-owned enterprises
3272:Democratic South Africa
2352:Encyclopædia Britannica
1865:Oxford University Press
1387:Equus quagga burchellii
1233:(eastern Lower Karoo).
1229:near Cranemere, in the
1009:that forms the base of
984: million years ago
240:vegetation consists of
4631:Geographical societies
4428:Landscape architecture
2903:Bunolagus monticularis
2660:8 January 2014 at the
2611:Accessed 30 April 2014
2555:Biomes of South Africa
2342:. Accessed 2014-04-24.
2284:. Space Today Online.
2054:The Plains of Camdeboo
1993:10.1098/rspb.2007.1370
1891:17 August 2021 at the
1785:Camdeboo National Park
1569:
1487:
1464:
1280:
1257:
1139:
1050:
930:
751:
602:
549:
458:Square Kilometer Array
341:
332:
32:Karoo (disambiguation)
4984:South African English
4423:Environmental studies
4395:Statistical geography
4276:Environmental science
3192:Kingdom of Mapungubwe
3012:Burman, Jose (1984).
2994:Conservation Genetics
2874:Biodiversity Explorer
2826:. Accessed 2 May 2014
2782:. Accessed 2 May 2014
2738:. Accessed 2 May 2014
2734:27 April 2014 at the
2717:. Accessed 2 May 2014
2664:. Accessed 2 May 2014
2490:"Rhebok Hiking Trail"
2338:26 April 2014 at the
2267:Bulpin, T.V. (1992).
1567:
1557:, and, of course, to
1481:
1461:
1271:
1251:
1137:
1091:, from approximately
1077:Succulent Karoo biome
1040:
908:
863:carnivorous therapsid
749:
599:
543:
425:and the Upper Karoo.
338:
314:
4636:Geoscience societies
4601:Interview (research)
4573:Land change modeling
4474:Computer cartography
4452:Techniques and tools
4310:Earth system science
3827:World Heritage Sites
3603:Water and sanitation
3212:Mthethwa Paramountcy
2917:: e.T3326A45176532.
2841:Animal Diversity Web
2683:The Nama Karoo Biome
2652:The Nama Karoo Biome
2567:Accessed 13 May 2014
2080:Conolly, D. (1992).
1886:English – Kora index
1645:, son of the famous
1219:Francois Le Vaillant
1182:), and sweet thorn (
1173:Rhigozum trichotomum
619:Waterberg Supergroup
615:Transvaal Supergroup
581:Geology of the Karoo
4793:Atmospheric science
4682:Spatial citizenship
4667:Geographers on Film
4657:Geography education
4267:Atmospheric science
3115:Karoo, South Africa
2563:25 May 2013 at the
2127:Geological Journeys
1863:(Online ed.).
1775:Karoo National Park
1770:People of the Karoo
1663:Karoo in literature
1375:Cape mountain zebra
1351:black-backed jackal
1125:Breede River Valley
1055:World Wildlife Fund
997:) ago. These "Enon
947:Great Wall of China
945:which resemble the
915:Cape Fold Mountains
611:Cape Fold Mountains
546:Swartberg Mountains
346:Cape Fold Mountains
321:Karoo National Park
121: /
4885:Quaternary science
4782:Physical geography
4563:Statistical survey
4513:Geologic modelling
4352:Quaternary science
3237:Transvaal Republic
3051:"The Dead Drummer"
2802:on 18 October 2014
2693:on 18 October 2014
2629:2 May 2014 at the
2607:5 May 2017 at the
2147:on 18 October 2014
2052:Palmer, E. (1966)
1647:Andrew Geddes Bain
1572:During the Second
1570:
1488:
1465:
1281:
1258:
1209:(particularly the
1179:Chrysocoma ciliata
1140:
1051:
931:
752:
719:Andrew Geddes Bain
603:
550:
482:Cape Fold Mountain
434:Verlatenkloof Pass
382:for Little Karoo.
374:It is called the
342:
333:
4946:
4945:
4880:Landscape ecology
4824:Coastal geography
4748:
4747:
4614:
4613:
4446:
4445:
4433:Landscape ecology
4253:Coastal geography
4013:
4012:
3973:
3972:
3616:
3615:
3608:Wealth inequality
3555:Income inequality
3502:
3501:
3477:Political parties
3442:Foreign relations
3404:
3403:
3301:
3300:
3232:Orange Free State
3207:Dutch Cape Colony
3197:Kingdom of Mutapa
2138:Grassland biome.
1871:(Subscription or
1687:South African War
1651:Bain's Kloof Pass
1379:Equus zebra zebra
1339:Verreaux's eagles
1309:African wild dogs
977:Cretaceous period
262:desert ephemerals
246:mesembryanthemums
150:
149:
16:(Redirected from
4991:
4934:
4933:
4922:
4910:
4909:
4897:
4815:Paleoclimatology
4775:
4768:
4761:
4752:
4751:
4736:
4735:
4724:
4723:
4712:
4700:
4699:
4528:Geovisualization
4457:
4456:
4400:Spatial analysis
4285:Paleoclimatology
4094:
4093:
4040:
4033:
4026:
4017:
4016:
3993:
3986:
3812:National symbols
3734:Social movements
3627:
3626:
3568:
3540:Economic history
3513:
3512:
3415:
3414:
3381:Populated places
3312:
3311:
3252:Great Depression
3168:
3167:
3144:
3137:
3130:
3121:
3120:
3102:
3087:
3081:
3079:
3077:
3061:
3055:
3054:
3043:
3037:
3030:
3024:
3010:
3004:
2986:
2980:
2973:
2967:
2960:
2954:
2947:
2936:
2935:
2933:
2931:
2926:
2896:
2890:
2889:
2887:
2885:
2866:
2857:
2856:
2854:
2852:
2833:
2827:
2825:
2819:
2811:
2809:
2807:
2798:. Archived from
2789:
2783:
2781:
2775:
2767:
2765:
2763:
2758:on 17 April 2014
2754:. Archived from
2745:
2739:
2724:
2718:
2716:
2710:
2702:
2700:
2698:
2689:. Archived from
2680:
2665:
2649:
2634:
2618:
2612:
2596:
2583:
2577:
2568:
2552:
2546:
2539:
2530:
2518:
2512:
2511:
2509:
2507:
2501:
2494:
2485:
2479:
2478:
2476:
2474:
2454:
2448:
2447:
2429:
2418:
2411:
2405:
2404:
2386:
2380:
2379:
2361:
2355:
2349:
2343:
2332:The Great Karoo
2330:
2324:
2323:
2321:
2319:
2304:
2298:
2297:
2295:
2293:
2278:
2272:
2265:
2226:
2219:
2196:
2190:
2171:
2170:
2164:
2156:
2154:
2152:
2143:. Archived from
2136:
2130:
2123:
2100:
2091:
2085:
2078:
2069:
2063:
2057:
2050:
2015:
2014:
2004:
1987:(1636): 759–65.
1972:
1966:
1960:
1923:
1916:
1895:
1883:
1877:
1876:
1868:
1856:
1849:
1843:
1837:
1755:
1740:
1725:
1713:
1698:
1508:Hex River valley
1383:Burchell's zebra
1355:Verreaux's eagle
1353:(6–10 kg),
1349:(7–19 kg),
1319:preyed on them.
1154:Nama Karoo biome
1071:Karoo Supergroup
1007:Malmesbury Group
992:
985:
923:Great Escarpment
715:palaeontologists
668:
652:
635:Karoo Supergroup
607:Karoo Supergroup
592:Karoo Supergroup
411:Hex River Valley
317:Great Escarpment
274:Great Escarpment
190:
184:
183:
180:
179:
176:
173:
170:
167:
164:
136:
135:
133:
132:
131:
126:
122:
119:
118:
117:
114:
94:Great Escarpment
86:
66:
42:
41:
21:
4999:
4998:
4994:
4993:
4992:
4990:
4989:
4988:
4949:
4948:
4947:
4942:
4898:
4889:
4819:Palaeogeography
4784:
4779:
4749:
4744:
4688:
4645:
4610:
4577:
4496:Distributed GIS
4442:
4404:
4356:
4289:Palaeogeography
4217:
4085:
4052:
4044:
4014:
4009:
3996:
3989:
3982:
3969:
3838:
3817:Public holidays
3748:
3714:Sexual violence
3694:Life expectancy
3612:
3566:
3560:Mining industry
3498:
3462:Law enforcement
3400:
3366:Mountain ranges
3297:
3276:
3247:Second Boer War
3157:
3148:
3095:
3090:
3086:of 5 June 1901.
3075:
3073:
3062:
3058:
3044:
3040:
3031:
3027:
3011:
3007:
2987:
2983:
2974:
2970:
2961:
2957:
2948:
2939:
2929:
2927:
2897:
2893:
2883:
2881:
2868:
2867:
2860:
2850:
2848:
2835:
2834:
2830:
2813:
2812:
2805:
2803:
2796:"Archived copy"
2794:
2792:Grassland Biome
2790:
2786:
2769:
2768:
2761:
2759:
2752:"Archived copy"
2750:
2746:
2742:
2736:Wayback Machine
2725:
2721:
2704:
2703:
2696:
2694:
2687:"Archived copy"
2685:
2681:
2668:
2662:Wayback Machine
2650:
2637:
2631:Wayback Machine
2621:Succulent Karoo
2619:
2615:
2609:Wayback Machine
2599:Succulent Karoo
2597:
2586:
2578:
2571:
2565:Wayback Machine
2553:
2549:
2540:
2533:
2519:
2515:
2505:
2503:
2499:
2492:
2486:
2482:
2472:
2470:
2455:
2451:
2444:
2430:
2421:
2412:
2408:
2401:
2387:
2383:
2376:
2362:
2358:
2350:
2346:
2340:Wayback Machine
2331:
2327:
2317:
2315:
2306:
2305:
2301:
2291:
2289:
2280:
2279:
2275:
2266:
2229:
2220:
2199:
2191:
2174:
2158:
2157:
2150:
2148:
2141:"Archived copy"
2139:
2137:
2133:
2124:
2103:
2092:
2088:
2079:
2072:
2064:
2060:
2051:
2018:
1973:
1969:
1961:
1926:
1917:
1898:
1893:Wayback Machine
1884:
1880:
1870:
1850:
1846:
1838:
1817:
1813:
1766:
1759:
1756:
1747:
1741:
1732:
1726:
1717:
1716:The Lower Karoo
1714:
1705:
1699:
1675:Rudyard Kipling
1665:
1617:
1469:Daniel Halladay
1429:
1424:
1371:
1331:riverine rabbit
1231:Camdeboo Plains
1203:
1198:
1162:
1156:
1129:Robertson Karoo
1085:
1083:Succulent Karoo
1079:
1063:succulent Karoo
1047:Succulent Karoo
1035:
987:
980:
956:
763:Karoo's geology
734:Stormberg Group
681:mud containing
678:
677:
676:
675:
674:
669:
660:
659:
658:
653:
644:
643:
637:
631:
594:
588:
586:The Great Karoo
583:
575:Plettenberg Bay
478:
423:Central Plateau
393:
388:
371:
363:Camdeboo Plains
354:Griqualand West
309:
293:
270:Kalahari Desert
188:
161:
157:
129:
127:
125:32.27°S 22.31°E
123:
120:
115:
112:
110:
108:
107:
101:
77:
57:
50:
47:
40:
35:
28:
23:
22:
15:
12:
11:
5:
4997:
4987:
4986:
4981:
4976:
4971:
4966:
4961:
4944:
4943:
4941:
4940:
4928:
4916:
4903:
4900:
4899:
4892:
4890:
4888:
4887:
4882:
4877:
4868:
4863:
4858:
4853:
4848:
4843:
4830:
4821:
4808:
4806:Phytogeography
4799:
4789:
4786:
4785:
4778:
4777:
4770:
4763:
4755:
4746:
4745:
4743:
4742:
4730:
4718:
4706:
4693:
4690:
4689:
4687:
4686:
4685:
4684:
4679:
4674:
4669:
4664:
4653:
4651:
4647:
4646:
4644:
4643:
4638:
4633:
4628:
4622:
4620:
4616:
4615:
4612:
4611:
4609:
4608:
4603:
4598:
4593:
4587:
4585:
4579:
4578:
4576:
4575:
4570:
4565:
4560:
4558:Remote sensing
4555:
4553:Photogrammetry
4550:
4545:
4540:
4535:
4530:
4525:
4520:
4518:Geomathematics
4515:
4510:
4509:
4508:
4503:
4498:
4488:
4483:
4482:
4481:
4476:
4465:
4463:
4454:
4448:
4447:
4444:
4443:
4441:
4440:
4438:Time geography
4435:
4430:
4425:
4420:
4414:
4412:
4406:
4405:
4403:
4402:
4397:
4392:
4387:
4382:
4380:Geoinformatics
4377:
4372:
4366:
4364:
4358:
4357:
4355:
4354:
4349:
4335:
4326:
4321:
4312:
4307:
4306:
4305:
4296:
4291:
4278:
4273:
4259:
4250:
4249:
4248:
4243:
4241:Phytogeography
4238:
4227:
4225:
4219:
4218:
4216:
4215:
4210:
4205:
4200:
4199:
4198:
4193:
4188:
4178:
4173:
4168:
4163:
4158:
4153:
4148:
4143:
4138:
4133:
4128:
4123:
4118:
4113:
4108:
4102:
4100:
4091:
4087:
4086:
4084:
4083:
4078:
4073:
4068:
4063:
4057:
4054:
4053:
4043:
4042:
4035:
4028:
4020:
4011:
4010:
4008:
4007:
4002:
3995:
3994:
3987:
3979:
3978:
3975:
3974:
3971:
3970:
3968:
3967:
3962:
3957:
3956:
3955:
3950:
3945:
3943:Cape Coloureds
3935:
3934:
3933:
3928:
3918:
3917:
3916:
3911:
3901:
3900:
3899:
3894:
3889:
3884:
3879:
3874:
3869:
3864:
3859:
3848:
3846:
3840:
3839:
3837:
3836:
3835:
3834:
3832:heritage sites
3824:
3819:
3814:
3809:
3804:
3799:
3794:
3789:
3784:
3774:
3769:
3764:
3758:
3756:
3750:
3749:
3747:
3746:
3741:
3736:
3731:
3726:
3721:
3719:Slum clearance
3716:
3711:
3706:
3701:
3696:
3691:
3686:
3681:
3676:
3671:
3666:
3661:
3656:
3651:
3646:
3641:
3636:
3630:
3624:
3618:
3617:
3614:
3613:
3611:
3610:
3605:
3600:
3595:
3590:
3585:
3580:
3578:Stock exchange
3575:
3570:
3562:
3557:
3552:
3547:
3542:
3537:
3535:Communications
3532:
3527:
3522:
3516:
3510:
3504:
3503:
3500:
3499:
3497:
3496:
3494:State security
3491:
3490:
3489:
3479:
3474:
3469:
3464:
3459:
3454:
3449:
3444:
3439:
3434:
3429:
3424:
3418:
3412:
3406:
3405:
3402:
3401:
3399:
3398:
3393:
3388:
3383:
3378:
3376:National parks
3373:
3371:Municipalities
3368:
3363:
3358:
3353:
3348:
3343:
3338:
3333:
3332:
3331:
3329:Climate change
3321:
3315:
3309:
3303:
3302:
3299:
3298:
3296:
3295:
3290:
3284:
3282:
3278:
3277:
3275:
3274:
3269:
3264:
3259:
3254:
3249:
3244:
3242:First Boer War
3239:
3234:
3229:
3224:
3219:
3214:
3209:
3204:
3199:
3194:
3189:
3184:
3183:
3182:
3171:
3165:
3159:
3158:
3147:
3146:
3139:
3132:
3124:
3118:
3117:
3112:
3107:
3094:
3093:External links
3091:
3089:
3088:
3056:
3038:
3025:
3005:
2981:
2968:
2955:
2937:
2891:
2858:
2828:
2784:
2740:
2719:
2666:
2635:
2613:
2584:
2569:
2547:
2531:
2513:
2480:
2449:
2443:0-947-008-02-0
2442:
2419:
2406:
2399:
2381:
2374:
2356:
2344:
2325:
2299:
2273:
2227:
2197:
2172:
2131:
2101:
2086:
2070:
2058:
2016:
1967:
1924:
1896:
1878:
1844:
1814:
1812:
1809:
1808:
1807:
1802:
1797:
1792:
1787:
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1760:
1757:
1750:
1748:
1742:
1735:
1733:
1727:
1720:
1718:
1715:
1708:
1706:
1700:
1693:
1664:
1661:
1636:Port Elizabeth
1616:
1613:
1574:Anglo-Boer War
1547:Port Elizabeth
1524:Eureka Diamond
1512:Matjiesfontein
1496:diamond fields
1484:Matjiesfontein
1428:
1425:
1423:
1422:Modern history
1420:
1370:
1367:
1287:, quagga, and
1202:
1199:
1197:
1194:
1176:), bitterbos (
1158:Main article:
1155:
1152:
1081:Main article:
1078:
1075:
1034:
1031:
1015:Cape Peninsula
1011:Table Mountain
955:
952:
903:
902:
891:
879:Massospondylus
875:
864:
852:
837:
825:
811:
808:Beaufort Group
799:
796:Beaufort Group
787:
784:Beaufort Group
775:
723:British Museum
703:Beaufort Group
670:
663:
662:
661:
654:
647:
646:
645:
641:
640:
639:
638:
633:Main article:
630:
627:
590:Main article:
587:
584:
582:
579:
567:Outeniqua Pass
559:Swartberg Pass
477:
474:
430:Matjiesfontein
392:
389:
387:
384:
370:
367:
308:
305:
292:
289:
218:natural region
148:
147:
142:
138:
137:
103:
102:
98:Cape Fold Belt
87:
79:
78:
70:Matjiesfontein
67:
59:
58:
56:Natural region
55:
52:
51:
48:
45:
38:
26:
9:
6:
4:
3:
2:
4996:
4985:
4982:
4980:
4977:
4975:
4972:
4970:
4967:
4965:
4962:
4960:
4957:
4956:
4954:
4939:
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4929:
4927:
4926:
4921:
4917:
4915:
4914:
4905:
4904:
4901:
4896:
4886:
4883:
4881:
4878:
4876:
4872:
4869:
4867:
4864:
4862:
4861:Geostatistics
4859:
4857:
4856:Geomorphology
4854:
4852:
4849:
4847:
4844:
4842:
4838:
4834:
4831:
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4771:
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4762:
4757:
4756:
4753:
4741:
4740:
4731:
4729:
4728:
4719:
4717:
4716:
4711:
4707:
4705:
4704:
4695:
4694:
4691:
4683:
4680:
4678:
4675:
4673:
4670:
4668:
4665:
4663:
4660:
4659:
4658:
4655:
4654:
4652:
4648:
4642:
4639:
4637:
4634:
4632:
4629:
4627:
4624:
4623:
4621:
4617:
4607:
4604:
4602:
4599:
4597:
4594:
4592:
4589:
4588:
4586:
4584:
4580:
4574:
4571:
4569:
4566:
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4559:
4556:
4554:
4551:
4549:
4546:
4544:
4541:
4539:
4536:
4534:
4531:
4529:
4526:
4524:
4523:Geostatistics
4521:
4519:
4516:
4514:
4511:
4507:
4504:
4502:
4499:
4497:
4494:
4493:
4492:
4489:
4487:
4486:Geochronology
4484:
4480:
4477:
4475:
4472:
4471:
4470:
4467:
4466:
4464:
4462:
4458:
4455:
4453:
4449:
4439:
4436:
4434:
4431:
4429:
4426:
4424:
4421:
4419:
4416:
4415:
4413:
4411:
4407:
4401:
4398:
4396:
4393:
4391:
4388:
4386:
4383:
4381:
4378:
4376:
4373:
4371:
4368:
4367:
4365:
4363:
4359:
4353:
4350:
4347:
4343:
4339:
4336:
4334:
4330:
4327:
4325:
4322:
4320:
4316:
4315:Geomorphology
4313:
4311:
4308:
4304:
4300:
4297:
4295:
4292:
4290:
4286:
4282:
4279:
4277:
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4268:
4265:
4264:
4263:
4262:Earth science
4260:
4258:
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4239:
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4129:
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4119:
4117:
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4109:
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4018:
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3808:
3805:
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3798:
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3775:
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3770:
3768:
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3760:
3759:
3757:
3755:
3751:
3745:
3742:
3740:
3737:
3735:
3732:
3730:
3729:Social issues
3727:
3725:
3722:
3720:
3717:
3715:
3712:
3710:
3707:
3705:
3702:
3700:
3697:
3695:
3692:
3690:
3687:
3685:
3682:
3680:
3679:Land invasion
3677:
3675:
3672:
3670:
3667:
3665:
3662:
3660:
3657:
3655:
3652:
3650:
3647:
3645:
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3581:
3579:
3576:
3574:
3571:
3569:
3563:
3561:
3558:
3556:
3553:
3551:
3550:Foreign trade
3548:
3546:
3543:
3541:
3538:
3536:
3533:
3531:
3528:
3526:
3523:
3521:
3518:
3517:
3514:
3511:
3509:
3505:
3495:
3492:
3488:
3485:
3484:
3483:
3480:
3478:
3475:
3473:
3470:
3468:
3465:
3463:
3460:
3458:
3455:
3453:
3450:
3448:
3445:
3443:
3440:
3438:
3435:
3433:
3430:
3428:
3425:
3423:
3420:
3419:
3416:
3413:
3411:
3407:
3397:
3394:
3392:
3389:
3387:
3384:
3382:
3379:
3377:
3374:
3372:
3369:
3367:
3364:
3362:
3359:
3357:
3354:
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3349:
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3344:
3342:
3339:
3337:
3334:
3330:
3327:
3326:
3325:
3322:
3320:
3317:
3316:
3313:
3310:
3308:
3304:
3294:
3291:
3289:
3286:
3285:
3283:
3279:
3273:
3270:
3268:
3265:
3263:
3260:
3258:
3255:
3253:
3250:
3248:
3245:
3243:
3240:
3238:
3235:
3233:
3230:
3228:
3225:
3223:
3220:
3218:
3215:
3213:
3210:
3208:
3205:
3203:
3200:
3198:
3195:
3193:
3190:
3188:
3187:Early history
3185:
3181:
3178:
3177:
3176:
3173:
3172:
3169:
3166:
3164:
3160:
3156:
3152:
3145:
3140:
3138:
3133:
3131:
3126:
3125:
3122:
3116:
3113:
3111:
3108:
3105:
3101:
3097:
3096:
3085:
3071:
3067:
3060:
3052:
3048:
3042:
3035:
3029:
3023:
3022:0-7981-1760-5
3019:
3015:
3009:
3003:
2999:
2995:
2991:
2985:
2978:
2972:
2965:
2959:
2952:
2946:
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2942:
2925:
2920:
2916:
2912:
2911:
2906:
2904:
2895:
2879:
2875:
2871:
2865:
2863:
2846:
2842:
2838:
2832:
2823:
2817:
2801:
2797:
2793:
2788:
2779:
2773:
2757:
2753:
2749:
2748:Savanna Biome
2744:
2737:
2733:
2730:
2728:
2723:
2714:
2708:
2692:
2688:
2684:
2679:
2677:
2675:
2673:
2671:
2663:
2659:
2656:
2653:
2648:
2646:
2644:
2642:
2640:
2632:
2628:
2625:
2622:
2617:
2610:
2606:
2603:
2600:
2595:
2593:
2591:
2589:
2581:
2576:
2574:
2566:
2562:
2559:
2556:
2551:
2544:
2538:
2536:
2528:
2527:0-520-24209-2
2524:
2517:
2498:
2491:
2484:
2468:
2464:
2463:New Scientist
2460:
2453:
2445:
2439:
2435:
2428:
2426:
2424:
2416:
2410:
2402:
2400:1-77007-148-2
2396:
2392:
2385:
2377:
2375:0-949956-26-0
2371:
2367:
2360:
2353:
2348:
2341:
2337:
2334:
2329:
2313:
2309:
2303:
2287:
2283:
2277:
2270:
2264:
2262:
2260:
2258:
2256:
2254:
2252:
2250:
2248:
2246:
2244:
2242:
2240:
2238:
2236:
2234:
2232:
2224:
2218:
2216:
2214:
2212:
2210:
2208:
2206:
2204:
2202:
2194:
2189:
2187:
2185:
2183:
2181:
2179:
2177:
2168:
2162:
2146:
2142:
2135:
2128:
2122:
2120:
2118:
2116:
2114:
2112:
2110:
2108:
2106:
2098:
2097:
2090:
2083:
2077:
2075:
2067:
2062:
2055:
2049:
2047:
2045:
2043:
2041:
2039:
2037:
2035:
2033:
2031:
2029:
2027:
2025:
2023:
2021:
2012:
2008:
2003:
1998:
1994:
1990:
1986:
1982:
1978:
1971:
1964:
1959:
1957:
1955:
1953:
1951:
1949:
1947:
1945:
1943:
1941:
1939:
1937:
1935:
1933:
1931:
1929:
1921:
1915:
1913:
1911:
1909:
1907:
1905:
1903:
1901:
1894:
1890:
1887:
1882:
1874:
1866:
1862:
1861:
1855:
1848:
1841:
1836:
1834:
1832:
1830:
1828:
1826:
1824:
1822:
1820:
1815:
1806:
1805:Karoo Ice Age
1803:
1801:
1798:
1796:
1793:
1791:
1788:
1786:
1783:
1781:
1778:
1776:
1773:
1771:
1768:
1767:
1754:
1749:
1746:
1739:
1734:
1731:
1730:Graaff-Reinet
1724:
1719:
1712:
1707:
1704:
1703:Beaufort West
1697:
1692:
1691:
1690:
1688:
1684:
1680:
1676:
1672:
1670:
1660:
1657:
1656:Meiringspoort
1652:
1648:
1644:
1639:
1637:
1632:
1628:
1626:
1622:
1612:
1610:
1605:
1603:
1599:
1598:Buffels River
1595:
1591:
1587:
1583:
1579:
1575:
1566:
1562:
1560:
1556:
1552:
1548:
1544:
1540:
1536:
1532:
1527:
1525:
1521:
1517:
1513:
1509:
1505:
1501:
1497:
1493:
1485:
1480:
1476:
1474:
1470:
1460:
1456:
1454:
1450:
1446:
1441:
1440:
1435:
1419:
1415:
1412:
1411:Graaff-Reinet
1406:
1404:
1400:
1396:
1390:
1388:
1384:
1380:
1376:
1366:
1364:
1360:
1359:martial eagle
1356:
1352:
1348:
1342:
1340:
1336:
1335:falconiformes
1332:
1327:
1324:
1320:
1318:
1314:
1310:
1306:
1302:
1298:
1292:
1290:
1286:
1279:
1275:
1270:
1266:
1264:
1263:Beaufort West
1255:
1250:
1246:
1244:
1240:
1236:
1232:
1228:
1224:
1220:
1216:
1212:
1208:
1193:
1191:
1190:Red Data Book
1187:
1186:
1185:Acacia karroo
1181:
1180:
1175:
1174:
1168:
1161:
1151:
1149:
1145:
1136:
1132:
1130:
1126:
1122:
1118:
1114:
1110:
1106:
1102:
1098:
1094:
1090:
1084:
1074:
1072:
1068:
1064:
1060:
1056:
1048:
1044:
1039:
1030:
1028:
1024:
1020:
1016:
1012:
1008:
1002:
1000:
999:Conglomerates
996:
990:
983:
978:
972:
970:
965:
962:
951:
948:
944:
940:
937:
928:
924:
920:
916:
912:
907:
901:
897:
896:
895:Megazostrodon
892:
889:
885:
881:
880:
876:
874:
870:
869:
865:
862:
858:
857:
853:
851:
847:
843:
842:
838:
835:
831:
830:
826:
824:
821:
817:
816:
812:
809:
805:
804:
800:
797:
793:
792:
788:
785:
781:
780:
776:
773:
772:
768:
767:
766:
764:
760:
757:
748:
744:
742:
737:
735:
730:
728:
724:
720:
716:
712:
708:
704:
700:
696:
695:KwaZulu-Natal
692:
688:
684:
673:
667:
657:
651:
636:
626:
624:
620:
616:
612:
608:
598:
593:
578:
576:
572:
568:
564:
563:Prince Albert
560:
554:
547:
542:
538:
536:
532:
528:
524:
520:
516:
512:
508:
504:
500:
495:
491:
487:
483:
473:
471:
467:
463:
459:
455:
451:
447:
443:
439:
435:
431:
426:
424:
420:
419:Beaufort West
416:
412:
407:
404:
402:
399:
383:
381:
377:
366:
364:
360:
355:
351:
347:
337:
330:
326:
325:Beaufort West
322:
318:
313:
304:
302:
298:
288:
285:
283:
280:, called the
279:
275:
271:
267:
263:
259:
255:
251:
247:
243:
239:
234:
231:
226:
223:
219:
216:
213:") is a semi-
212:
208:
204:
200:
197:
193:
192:
182:
155:
146:
143:
139:
134:
130:-32.27; 22.31
106:Coordinates:
104:
99:
95:
91:
85:
80:
75:
71:
65:
60:
53:
43:
37:
33:
19:
4935:
4923:
4911:
4833:Soil science
4828:Oceanography
4802:Biogeography
4737:
4725:
4713:
4701:
4662:Geo-literacy
4619:Institutions
4501:Internet GIS
4461:Quantitative
4338:Soil science
4257:Oceanography
4246:Zoogeography
4231:Biogeography
4106:Agricultural
3844:Demographics
3792:Homelessness
3762:Architecture
3593:Trade unions
3452:Human rights
3422:Constitution
3319:Biodiversity
3257:World War II
3227:Zulu Kingdom
3151:South Africa
3074:. Retrieved
3064:Mary Hamer.
3059:
3047:Thomas Hardy
3041:
3033:
3028:
3013:
3008:
2993:
2989:
2984:
2976:
2971:
2963:
2958:
2950:
2928:. Retrieved
2914:
2908:
2902:
2894:
2882:. Retrieved
2873:
2849:. Retrieved
2840:
2831:
2804:. Retrieved
2800:the original
2791:
2787:
2760:. Retrieved
2756:the original
2747:
2743:
2727:Fynbos Biome
2726:
2722:
2695:. Retrieved
2691:the original
2682:
2651:
2620:
2616:
2598:
2579:
2554:
2550:
2542:
2516:
2504:. Retrieved
2483:
2471:. Retrieved
2462:
2452:
2433:
2414:
2409:
2390:
2384:
2365:
2359:
2351:
2347:
2328:
2316:. Retrieved
2302:
2290:. Retrieved
2276:
2268:
2222:
2192:
2149:. Retrieved
2145:the original
2134:
2126:
2094:
2089:
2081:
2065:
2061:
2053:
1984:
1980:
1970:
1962:
1919:
1881:
1858:
1847:
1839:
1673:
1669:Thomas Hardy
1666:
1649:, who built
1640:
1633:
1629:
1620:
1618:
1606:
1571:
1559:Johannesburg
1551:Bloemfontein
1528:
1489:
1466:
1437:
1430:
1416:
1407:
1391:
1386:
1378:
1372:
1343:
1328:
1325:
1321:
1293:
1282:
1259:
1223:hippopotamus
1204:
1183:
1177:
1171:
1167:fynbos biome
1163:
1141:
1121:Tankwa Karoo
1113:Orange River
1109:Richtersveld
1093:Lamberts Bay
1086:
1052:
1019:Western Cape
1003:
973:
957:
932:
900:early mammal
893:
877:
866:
854:
848:herbivorous
841:Lystrosaurus
839:
827:
813:
801:
789:
777:
769:
753:
738:
731:
727:Robert Broom
679:
672:Lystrosaurus
671:
655:
604:
555:
551:
531:Amalienstein
484:ranges, the
479:
427:
413:just before
408:
405:
394:
375:
372:
359:Tankwa Karoo
343:
294:
286:
282:Tankwa Karoo
235:
227:
206:
153:
151:
145:South Africa
90:South Africa
36:
4974:Namaqualand
4811:Climatology
4797:Meteorology
4739:WikiProject
4591:Ethnography
4583:Qualitative
4543:Map algebra
4538:Hydrography
4479:Web mapping
4469:Cartography
4281:Climatology
4271:Meteorology
4126:Development
3948:Cape Malays
3669:Immigration
3520:Agriculture
3341:Earthquakes
3222:Cape Colony
3202:Kaditshwene
2990:Equus zebra
2930:12 November
2884:17 November
2851:17 November
2697:18 December
2488:Footprint.
1683:Dwyka River
1643:Thomas Bain
1625:Cango Caves
1615:Klein Karoo
1594:blockhouses
1582:Cape Colony
1492:Cape Colony
1427:Great Karoo
1369:Klein Karoo
1201:Great Karoo
1196:Karoo fauna
1105:Namaqualand
1033:Karoo flora
1027:Cango Caves
856:Thrinaxodon
803:Procolophon
798:insectivore
779:Bradysaurus
687:Dwyka Group
656:Bradysaurus
535:Dysselsdorp
476:Klein Karoo
470:earthquakes
442:Mpumalangan
415:Touws River
391:Great Karoo
378:, which is
376:Klein Karoo
369:Klein Karoo
350:Bushmanland
307:Great Karoo
266:Bushmanland
128: /
72:, with the
18:Klein Karoo
4953:Categories
4866:Glaciology
4846:Geobiology
4841:Edaphology
4596:Geopoetics
4410:Integrated
4346:Edaphology
4324:Glaciology
4299:Geophysics
4294:Geobiology
4181:Settlement
4171:Population
4141:Historical
4111:Behavioral
4071:Philosophy
3926:Afrikaners
3914:San people
3797:Literature
3744:Xenophobia
3664:Healthcare
3644:Disability
3567:(currency)
3472:Parliament
3447:Government
3432:Corruption
3267:Border War
2318:28 January
2292:28 January
2099:116: 1–54.
1875:required.)
1811:References
1679:blockhouse
1609:game farms
1602:Laingsburg
1239:wildebeest
1227:rhinoceros
1160:Nama Karoo
1144:Asteraceae
1089:West Coast
1067:Nama Karoo
961:quartzitic
911:Calitzdorp
868:Euparkeria
771:Mesosaurus
711:amphibians
699:Ecca Group
683:dropstones
519:Oudtshoorn
515:Calitzdorp
438:Sutherland
254:euphorbias
238:xerophytic
4875:Limnology
4871:Hydrology
4650:Education
4568:Surveying
4390:Geomatics
4370:Geodesign
4362:Technical
4333:Limnology
4329:Hydrology
4208:Strategic
4191:Transport
4166:Political
4156:Marketing
4116:Cognitive
4047:Geography
3938:Coloureds
3684:Languages
3649:Education
3598:Transport
3530:Companies
3482:President
3437:Elections
3386:Provinces
3346:Estuaries
3336:Districts
3307:Geography
3262:Apartheid
3084:The Times
2506:13 August
1590:guerrilla
1504:Worcester
1500:Kimberley
1467:In 1854,
1439:trekboers
1434:Algoa Bay
1274:springbok
1254:Louis XVI
1243:ostriches
1211:springbok
1127:, as the
1023:limestone
969:Bokkeveld
964:sandstone
927:Swartberg
886:to early
873:archosaur
850:therapsid
815:Diictodon
786:herbivore
601:purposes.
571:Langkloof
511:Ladismith
507:Barrydale
494:Outeniqua
490:Langeberg
486:Swartberg
466:Milky Way
454:Carnarvon
436:to reach
386:Geography
380:Afrikaans
291:Divisions
258:stapelias
250:crassulas
207:ǃ’Aukarob
199:!Orakobab
49:ǃ’Aukarob
4913:Category
4837:Pedology
4703:Category
4342:Pedology
4223:Physical
4186:Regional
4176:Religion
4161:Military
4151:Language
4146:Internet
4131:Economic
4121:Cultural
4090:Branches
4061:Glossary
4000:Category
3909:Khoekhoe
3787:HIV/AIDS
3709:Religion
3674:Intersex
3654:Feminism
3634:Cannabis
3583:Taxation
3487:timeline
3467:Military
3410:Politics
3396:Wildlife
3293:Military
3281:By topic
3217:Ndwandwe
3175:Timeline
3155:articles
3076:22 April
3070:Archived
3049:(1899).
2878:Archived
2845:Archived
2816:cite web
2772:cite web
2732:Archived
2707:cite web
2658:Archived
2627:Archived
2605:Archived
2561:Archived
2497:Archived
2467:Archived
2336:Archived
2312:Archived
2286:Archived
2161:cite web
2011:18198148
1889:Archived
1764:See also
1586:Calvinia
1578:commando
1535:Zimbabwe
1531:Botswana
1520:Hopetown
1473:windpump
1463:Koppies.
1363:Leopards
1305:cheetahs
1301:leopards
1278:gazelles
1235:Elephant
1207:antelope
1101:sandveld
1065:and the
979:, about
936:dolerite
888:Jurassic
884:Triassic
861:Triassic
846:Triassic
836:predator
829:Rubidgea
823:synapsid
810:omnivore
791:Owenetta
756:dolerite
741:volcanic
707:reptiles
623:Gondwana
398:dolerite
329:dolerite
276:and the
230:Highveld
203:Khoemana
196:Khoekhoe
74:Anysberg
4937:Commons
4851:Geology
4727:Commons
4506:Web GIS
4375:Geodesy
4319:Geology
4303:Geodesy
4236:Ecology
4213:Tourism
4081:Outline
4066:History
3984:Outline
3965:Chinese
3960:Indians
3953:Griquas
3931:British
3904:Khoisan
3857:Ndebele
3777:Cuisine
3754:Culture
3724:Smoking
3699:Poverty
3622:Society
3588:Tourism
3525:Banking
3508:Economy
3356:Islands
3351:Forests
3324:Climate
3288:Economy
3163:History
2473:23 June
2002:2596898
1854:"karoo"
1745:Cradock
1543:Namibia
1399:Cradock
1347:caracal
1317:jackals
1285:blesbok
1213:), the
1148:lucerne
1117:Namibia
1097:Namibia
1013:on the
993:years (
991:million
882:, late
834:Permian
820:Permian
691:tillite
523:De Rust
503:Montagu
499:defiles
319:in the
222:geology
141:Country
116:22°19′E
113:32°16′S
4925:Portal
4715:Portal
4203:Social
4136:Health
4050:topics
4005:Portal
3921:Whites
3882:Tswana
3877:Tsonga
3822:Sports
3772:Cinema
3704:Racism
3659:Health
3545:Energy
3427:Courts
3391:Rivers
3153:
3020:
2525:
2440:
2397:
2372:
2009:
1999:
1555:Durban
1539:Zambia
1516:De Aar
1315:, and
1313:hyenas
1215:quagga
1107:, the
1059:biomes
1043:biomes
533:, and
521:, and
464:, the
462:galaxy
260:, and
215:desert
4959:Karoo
4196:Urban
4098:Human
4076:Index
3991:Index
3892:Xhosa
3887:Venda
3872:Swazi
3867:Sotho
3807:Music
3802:Media
3739:Women
3639:Crime
3565:Rand
3361:Lakes
3180:Years
3104:Karoo
2806:2 May
2762:2 May
2500:(PDF)
2493:(PDF)
2151:2 May
1869:
1667:Poet
1621:kango
1397:near
1297:lions
1289:eland
943:dikes
939:sills
759:sills
401:sills
323:near
242:aloes
209:"Hard
205:word
154:Karoo
46:Karoo
3897:Zulu
3862:Pedi
3781:wine
3689:LGBT
3078:2012
3018:ISBN
2932:2021
2915:2019
2886:2017
2853:2017
2822:link
2808:2014
2778:link
2764:2014
2713:link
2699:2014
2523:ISBN
2508:2006
2475:2009
2438:ISBN
2395:ISBN
2370:ISBN
2320:2009
2294:2009
2167:link
2153:2014
2007:PMID
1545:and
1537:and
1445:Khoe
1337:and
1329:The
1241:and
1053:The
709:and
617:and
527:Zoar
236:The
211:veld
152:The
3767:Art
3457:Law
2998:doi
2919:doi
1997:PMC
1989:doi
1985:275
1498:in
1453:Ntu
1449:!Ui
1377:, (
986:to
982:145
201:or
189:ROO
187:kə-
4955::
4873:/
4839:/
4835:/
4826:/
4817:/
4813:/
4804:/
4795:/
4331:/
4317:/
4301:/
4287:/
4283:/
4269:/
4255:/
3068:.
2996:.
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2876:.
2872:.
2861:^
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2839:.
2818:}}
2814:{{
2774:}}
2770:{{
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794:,
782:,
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537:.
529:,
517:,
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509:,
505:,
256:,
252:,
248:,
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2529:.
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2446:.
2403:.
2378:.
2322:.
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2013:.
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181:/
178:ə
175:u
172:r
169:ˈ
166:ə
163:k
160:/
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