Eleven countries have only a single site each. Four sites are shared between two countries: However, there are around a dozen archaeological sites in the country that are believed to be potential future candidates for World Heritage status. Selection is based on ten criteria: In Africa, there are 85 cultural, 45 natural, and 5 mixed sites. It planned to protect the sites by hiring personnel for state parties to maintain national inventories of existing sites, as well as to “prepare nomination dossiers for inscription onto the World Heritage List. The Democratic Republic of Congo and Libya both have 5 sites on the danger list, the second highest of any country in the world and two of the three countries to have more than three sites inscribed. The table is sortable by column by clicking on the at the top of the appropriate column; alphanumerically for the Site, Area, and Year columns; by state party followed by the region for the Location column; and by criteria type followed by the country for the Criteria column. Site — named after the World Heritage Committee’s official designation [1] Location — sorted by country, followed by the region at the regional or provincial level.

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Please report a broken link to [email protected] Books and CDs. The Van Riebeeck Society – Makes primary sources in South African history available in a readable and enjoyable form to anyone interested in Southern African history.. Societies. Cape Town Family History Society – A go getter genealogical society, with the accent on Cape families and history.

Questions about your old globe? Want to see photos of antique and vintage world globes? Do you collect antique or vintage terrestrial globes? Perhaps you like to see how older world globes show the political boundaries of their times. It is fascinating to see how countries and cities have changed their names over the decades, and the results of wars that have moved boundaries. Some people collect globes because they often show the tracks and routes that explorers took as they learned about our planet.

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Looking at it makes one wonder what it is that holds so much fascination for them. But after a while one realizes that there is more than meets the eye and that the first impression of a desolated ancient land only goes surface deep. Northern Province certainly has its own unique attractiveness amid the other South African provinces. Below that seemingly desolate surface great riches is has been found in the form of large deposits gem stones such as topaz, opal, garnet, jasper, rose quarts, agate and last but certainly not least, diamonds.

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The reasons are historical. In the mid-seventeenth century, Dutch settlers began to occupy the part of South Africa now known as the Western Cape. South African law reflects this history of successive colonial governance. The ‘common law’ of the country in this context, ‘common law’ implies law of non-statutory origin is based on the ‘Roman-Dutch’ law of the original Dutch settlers. This is civilian law – Roman law as interpreted by the Dutch writers of the 17th and 18th centuries.

Thus originally, important primary sources of South African law were the treatises of authors such as Grotius, Johannes Voet, Simon Groenewegen and Johannes van der Linden. Law was modified or expanded by statute. When the British took possession of the Cape in they did not impose their substantive legal system in a formal way. Instead, it was decided that the local Roman-Dutch law would remain in force.

However, English procedural law was adopted and this had a tendency to influence substantive provisions.

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Life Size, Accurate and artistic: Pre-Historic animals – open 7 days a week. The Sudwala Dinosaur Park offers children an exciting and educational glimpse into the world of Dinosaurs and other pre-historic animals. It is situated next to the Sudwla Caves in a lush, sub-tropical forest garden where beautiful cabbage trees, cycads, monkeys and birds abound. Through countless eons the swirling whirlpools which occur as the Treur River plunges into the Blyde River, caused waterborne sand and rock to grind huge, cylindrical potholes into the bedrock of the river.

The Potholes were named after a gold digger, Tom Bourke, who staked a claim nearby.

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However, the temporally discontinuous nature of this evidence precludes ready assumptions of intrinsic adaptive benefit, and has encouraged diverse explanations for the occurrence of these behaviors, in terms of regional demographic, social and ecological conditions. Here, we present a new high-resolution multi-proxy record of environmental change that indicates that faunal exploitation patterns and lithic technologies track climatic variation across the last 22, years in the southern Cape.

Conditions during the Last Glacial Maximum and deglaciation were humid, and zooarchaeological data indicate high foraging returns. By contrast, the Holocene is characterized by much drier conditions and a degraded resource base. Critically, we demonstrate that systems for technological delivery — or provisioning — were responsive to changing humidity and environmental productivity. However, in contrast to prevailing models, bladelet-rich microlithic technologies were deployed under conditions of high foraging returns and abandoned in response to increased aridity and less productive subsistence environments.

This suggests that posited links between microlithic technologies and subsistence risk are not universal, and the behavioral sophistication of human populations is reflected in their adaptive flexibility rather than in the use of specific technological systems. Previous article in issue.

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The project involved the excavation of a number of rock shelters in the Grahamstown area, including Wilton Large Rockshelter and Cave, Glen Craig, Roodekrantz, and Spitzkop. Hewitt himself was also involved in excavations at Melkhoutboom, as well as Middelkop, Tefelburg Hall, and several sites near the Kabeljous River Mouth. The cave is situated within a steep ravine in the Cape Folded Mountain Belt, a range of mountains that marks the boundary between the more tropical ecological zone of the inland Karoo and the coastal plain.

The coastal strip consists mostly of sand beaches bordered by dunes to the north. There is little vegetation, and subsistence in this area during the Later Stone Age likely consisted mainly of shellfish — as evidenced by the abundance of shell middens dating to within the last 12, years — as well as fish, crustaceans, great white sharks, and birds. This area consists mainly of grassland and shrubland, and contains many succulents and other edible plants and shrubs.

This area contains grassland, shrubland, fynbos , and scree forest, all with a variety of vegetation; the fauna is equally varied, consisting of antelope including grysbok, duiker, and bushbuck , wild pigs, and other small- to medium-sized mammals. This area has a much drier climate than the zones farther south; severe droughts are common, and this was likely the case in the Middle Stone Age as well, affecting habitability in this area.

A variety of large mammals, such as rhinoceros, elephants, hippopotamus, wildebeest, eland, and large antelope, used to inhabit this area but have since migrated or gone extinct due to changes in indigenous vegetation caused by overgrazing. The environment within the ravine can be described as evergreen temperate forest, and there is a diverse assortment of vegetation throughout the ravine and the surrounding area, including tall trees throughout the ravine and surrounding the opening of the cave, which is about 6 meters above the floor of the ravine.

At the back of the main cave is a higher, smaller cave that shows some evidence of occupation in the form of ash and scattered artifacts, but has not been excavated. The subsequent excavation in was planned based on this initial excavation, extending and building upon it. Both excavations used the same grid system running north-south and east-west. This was primarily due to constraints on time and resources, which stopped excavation from being extended to promising areas or even bringing the whole of the excavated area down to bedrock; instead, efforts were focused on obtaining a large sample of artifacts and floral and faunal remains from the area already excavated.

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History The prehistory and history of South Africa span nearly the entire known existence of human beings and their ancestors—some three million years or more—and include the wandering of small bands of hominins through the savanna , the inception of herding and farming as ways of life, and the construction of large urban centres. Through this diversity of human experience, several trends can be identified: This article focuses on the country of South Africa. For information about the country in its regional context , see Southern Africa.

The first specimen of these hominins to be found in was the skull of a child from a quarry site at Taung in what is now the North-West province. Subsequently more australopithecine fossils were discovered in limestone caves farther northeast at Sterkfontein , Swartkrans , and Kromdraai collectively designated a World Heritage site in , where they had originally been deposited by predators and scavengers.

The primary distinction is between a reliance on chipped and flaked stone implements the Stone Age and the ability to work iron the Iron Age. The simple stone tools found with australopithecine fossil bones fall into the earliest part of the Early Stone Age.

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