Clarens | |
---|---|
Coordinates: 28°31′S28°25′E / 28.517°S 28.417°E | |
Country | South Africa |
Province | Free State |
District | Thabo Mofutsanyane |
Municipality | Dihlabeng |
Government | |
• Type | Municipality |
• Mayor | Tjhetane Mofokeng [1] (ANC) |
Area | |
• Total | 13.7 km2 (5.3 sq mi) |
Population (2011) [2] | |
• Total | 751 |
• Density | 55/km2 (140/sq mi) |
Racial makeup (2011) | |
• White | 58.32% |
• Black African | 34.09% |
• Coloured | 4.13% |
• Indian/Asian | 3.20% |
• Other | 0.27% |
First languages (2011) | |
• English | 44.02% |
• Afrikaans | 46.37% |
• Sotho | 7.05% |
• Other | 2.56% |
Time zone | UTC+2 (SAST) |
Postal code (street) | 9707 |
PO box | 9707 |
Area code | 058 |
Clarens is a small town situated in the foothills of the Maluti Mountains in the Free State province of South Africa and nicknamed the "Jewel of the Eastern Free State". It was established in 1912 and named after the town of Clarens in Switzerland where exiled Paul Kruger spent his last days. It is situated 336 km from Johannesburg, 284 km from Bloemfontein, and 389 km from Durban.
A farm called "Leliehoek" (English: Lily Corner) was bought from Hermanus Steyn in 1910, and in 1911 Piet de Villiers sold his farm "Naauwpoort" (situated near the Titanic rock) to a company that planned to establish a village there. These two farms were divided into stands and sold for fifty pounds each.
A commission was appointed in 1912 to finalise negotiations, and a decision was made to name the village "Clarens" in honour of President Paul Kruger’s influence in the area. This came about in the following way - during the Free State-Basotho War of 1865 - 1866, five burghers (citizens) of the Transvaal were murdered in the Eastern Free State, and as a result war was declared against the Basotho leader, Moshoeshoe.
Paul Kruger, together with a commando of burghers, defeated the Basotho at the Battle of Naauwpoortnek (near Titanic rock). President Kruger spent his last days as a voluntary exile in the attractive village of Clarens in Switzerland, and thus Clarens was named for this Swiss town. A monument was erected on the farm "Ararat" just outside Clarens, in honour of the five burghers murdered by the Basotho on 29 September 1865, during the siege of Naauwpoort. This monument was later moved to Clarens and placed in the central town square, where it stands to this day.
Clarens is an artists' haven with many well-known artists either living in or frequenting the village, with many art galleries scattered around the village square and the town. The tranquil village ambience combined with scenic views and a mild climate has made Clarens a popular getaway for city dwellers from Johannesburg, Bloemfontein and Durban, among other places. Clarens is known for its spectacular sandstone mountains and wonderful climate; it is one of the most picturesque spots in South Africa and has recently been acclaimed as the best Trout Fishing waters in South Africa.
The Golden Gate Highlands National Park with its sandstone formations and cliffs is 17 km from Clarens.
Close to Clarens is the outlet from the Lesotho Highlands Water Project that brings fresh water from Lesotho to feed into the As River (Afrikaans for "axle" because a wagon broke its axle when crossing, but has been mistakenly translated into English as "ash"), Liebenbergsvlei and Wilge Rivers feed into the Vaal Dam. Water from the Vaal Dam is then abstracted, treated and pumped to the Rand Water supply area.
Clarens is part of the scenic Highlands Route and is surrounded by mountains. The Rooiberge is the range encompassing the village, while further towards the southeast are the Maluti mountains in shades of purple and blue. All around are the sandstone cliffs with their multi-coloured layers - these horizontal strata are a characteristic feature of the area. Many homes in the Clarens Valley are made from or clad in sandstone.
There are various establishments offering accommodation, including bed & breakfasts, self-catering, lodges, backpackers and farm guest houses in the surrounding area.
Activities include: horse riding, abseiling, hiking, fly-fishing, fossil hunting, white-water rafting and golf. Live music is often performed on weekends.
Large Jurassic dinosaurs lived in the eastern part of Free State about 200-million-years ago, when the giant southern super-continent, Gondwana, was still intact. [3]
From 12 January 2009 the remains of the largest dinosaurs ever to be found on South African soil were discovered in Clarens, a small town in Free State (province). Dr Jonah Choineire, a senior researcher at the Evolutionary Studies Institute, said the remains of the large creature were found between the border of Lesotho and South Africa just outside of Clarens. [4]
The remains were discovered at a construction site of the Ingula Pump and Storage Scheme, developed by Eskom Holdings (Pty) Ltd. Gavin Anderson, the project archaeologist, together with Dr Gideon Groenewald, a geologist/palaeontologist, was requested to assist with the recording of fossil finds at the construction site. The sites of the excavations were inspected on a continuous basis during the excavation on 12 January 2009. Up to 2017, twenty five sites have been recorded, where fossilised bone were found. Remains of the vertebrates discovered were very broken and unfortunately disturbed by the excavations.
A very well-preserved tusk of a plant-eating reptile, possibly a Dicynodon lacerticeps, was later recorded. The discovery of well-preserved bone fossils in the main quarry indicated that the interbedded mudstones in the region might have provided valuable information on the fauna of the ancient environment in that region. [5]
Eskom Holdings donated a container for the storage of fossils on site. Temporary curation of fossils was supplied for that storage. The Gorgonopsid and other fossils recorded up to 31 January 2009 were then transported to the National Museum in Bloemfontein on 11 March 2009. [5]
The team discovered the remains of the largest dinosaur to walk in the southern parts of Africa, [6] namely a 190-million-year-old fossilised egg of a Massospondylus dinosaur. This dinosaur lived in the Late Triassic and Early Jurassic, a period from about 230-million years ago to about 185-million years ago. The Massospondylus wandered about in great herds, migrating back and forth between what would, millions of years later, become Southern Africa and Russia, when the southern super-continent, Gondwana, was still intact. The rocks that were laid down during this period are called the Stormberg Group of rocks, and it is in rocks of the Stormberg Group that the fossils of Massospondylus and other dinosaurs were found. [3] Massospondylus dinosaurs hatched from eggs not much larger than a hen’s egg, but grew into big creatures 5 to 6 metres long. [7] They had large bodies, long necks and small heads, and long tails. [8]
Another species found was a 210-million-year-old sauropod named Antetonitrus. It was found in the Ladybrand District of the Free State (province). The dinosaurs dominated the region for about 120-million years until the end of the Cretaceous Period, 65-million years ago. [8]
The Orange Free State was an independent Boer-ruled sovereign republic under British suzerainty in Southern Africa during the second half of the 19th century, which ceased to exist after it was defeated and surrendered to the British Empire at the end of the Second Boer War in 1902. It is one of the three historical precursors to the present-day Free State province.
Smithfield is a small town in the Free State province of South Africa. Founded in 1848 in the Orange River Sovereignty, the town is situated in a rural farming district and is the third oldest town in present-day Free State, after Philippolis and Winburg.
Massospondylus was a genus of sauropodomorph dinosaur from the Early Jurassic. It was described by Sir Richard Owen in 1854 from remains discovered in South Africa, and is thus one of the first dinosaurs to have been named. Fossils have since been found at other locations in South Africa, Lesotho, and Zimbabwe. Material from Arizona's Kayenta Formation, India, and Argentina has been assigned to the genus at various times, but the Arizonan and Argentinian material are now assigned to other genera.
The Karoo Supergroup is the most widespread stratigraphic unit in Africa south of the Kalahari Desert. The supergroup consists of a sequence of units, mostly of nonmarine origin, deposited between the Late Carboniferous and Early Jurassic, a period of about 120 million years.
Golden Gate Highlands National Park is located in Free State, South Africa, near the Lesotho border. It covers an area of 340 km2 (130 sq mi). The park's most notable features are its golden, ochre, and orange-hued, deeply eroded sandstone cliffs and outcrops, especially the Brandwag rock. Another feature of the area is the numerous caves and shelters displaying San rock paintings. Wildlife featured at the park includes mongooses, eland, zebras, and over 100 bird species. It is the Free State's only national park and is more famous for the beauty of its landscape than for its wildlife. Numerous palaeontology finds have been made in the park, including dinosaur eggs and skeletons.
Dracovenator is a genus of neotheropod dinosaur that lived approximately 201 to 199 million years ago during the early part of the Jurassic Period in what is now South Africa. Dracovenator was a medium-sized, moderately-built, ground-dwelling, bipedal carnivore, that could grow up to an estimated 5.5–6.5 metres (18–21 ft) in length and 250 kilograms (550 lb) in body mass. Its type specimen was based on only a partial skull that was recovered.
The Clarens Formation is a geological formation found in several localities in Lesotho and in the Free State, KwaZulu-Natal, and Eastern Cape provinces in South Africa. It is the uppermost of the three formations found in the Stormberg Group of the greater Karoo Supergroup rocks and represents the final phase of preserved sedimentation of the Karoo Basin.
The Bushveld Sandstone is a geological formation dating to roughly between 201 and 189 million years ago and covering the Carnian to Norian stages. The Bushveld Sandstone is found in Transvaal, South Africa, and is a member of the Stormberg Group. As its name suggests, it consists mainly of sandstone. Fossils of the prosauropod dinosaur Massospondylus have been recovered from the Bushveld Sandstone.
The Elliot Formation is a geological formation and forms part of the Stormberg Group, the uppermost geological group that comprises the greater Karoo Supergroup. Outcrops of the Elliot Formation have been found in the northern Eastern Cape, southern Free State, and in the eastern KwaZulu-Natal provinces of South Africa. Outcrops and exposures are also found in several localities in Lesotho such as Qacha's Neck, Hill Top, Quthing, and near the capital, Maseru. The Elliot Formation is further divided into the lower (LEF) and upper (UEF) Elliot formations to differentiate significant sedimentological differences between these layers. The LEF is dominantly Late Triassic (Norian-Hettangian) in age while the UEF is mainly Early Jurassic (Sinemurian-Pliensbachian) and is tentatively regarded to preserve a continental record of the Triassic-Jurassic boundary in southern Africa. This geological formation is named after the town of Elliot in the Eastern Cape, and its stratotype locality is located on the Barkly Pass, 9 km north of the town.
The Molteno Formation is a geological formation found in several localities in Lesotho and South Africa. It lies mainly south of Maseru, near Burgersdorp, Aliwal North, Dordrecht, Molteno, and Elliot. It extends as far north as Matatiele in the Eastern Cape. The formation's localities lie along the Drakensberg Mountains in Kwazulu-Natal, and near Ladybrand in the Free State of South Africa. The Molteno Formation is the lowermost of the three formations in the Stormberg Group of the greater Karoo Supergroup. The Molteno Formation represents the initial phase of preserved sedimentation of the Stormberg Group.
Ignavusaurus is a genus of basal sauropodomorph dinosaur that lived during the Early Jurassic in what is now Lesotho. Its fossils were found in the Upper Elliot Formation which is probably Hettangian in age. It was described on the basis of a partial, well preserved articulated skeleton. The type species, I. rachelis, was described in 2010 by Spanish palaeontologist F. Knoll.
The Stormberg Group is one of the four geological groups that comprises the Karoo Supergroup in South Africa. It is the uppermost geological group representing the final phase of preserved sedimentation of the Karoo Basin. The Stormberg Group rocks are considered to range between Lower Triassic (Olenekian) to Lower Jurassic (Pliensbachian) in age. These estimates are based on means of geological dating including stratigraphic position, lithostratigraphic and biostratigraphic correlations, and palynological analyses.
Maluti-a-Phofung Municipality is a local municipality within the Thabo Mofutsanyane District Municipality, in the Free State province of South Africa. It encompasses substantially all of the former bantustan of QwaQwa, except for the small enclave at Botshabelo. The population is almost entirely Basotho. The municipality is named after the Drakensberg mountains. The peak is known as the Sentinel, which is called Phofung in Sesotho.
Pegomastax is a genus of heterodontosaurid dinosaur that lived during the Early Jurassic of South Africa. The only known specimen was discovered in a 1966–1967 expedition in Transkei District of Cape Province, but was not described until 2012 when Paul Sereno named it as the new taxon Pegomastax africana. The genus name is derived from the Greek for "strong jaw", and the species name describes the provenance of Africa; it was originally spelled africanus, was corrected to africana to align with the gender of the genus name.
For thousands of years, a pilgrimage has been made by the Basotho people to a network of sacred caves to communicate with the spiritual world. The caves also contain dinosaur footprints and ancient rock paintings. The caves are located between the eastern parts of the Free State and Lesotho. These sacred caves are often described as 'the key to religion' in Southern Africa.
The Battle of Naauwpoort Nek refers to a clash between the Trekboers and Basotho warriors on 29 September 1865. Naauwpoort lies immediately to the north of the Free State town of Clarens.
The geology of Lesotho is built on ancient crystalline basement rock up to 3.6 billion years old, belonging to the Kaapvaal Craton, a section of stable primordial crust. Most of the rocks in the country are sedimentary or volcanic units, belonging to the Karoo Supergroup. The country is notable for large fossil deposits and intense erosion due to high rainfall and a rare case of southern African glaciation during the last ice age. Lesotho has extensive diamonds and other natural resources and has the highest concentration of kimberlite pipes anywhere in the world.
Ngwevu is a genus of massospondylid sauropodomorph dinosaur from the Lower Jurassic of South Africa. The genus contains one species, Ngwevu intloko.
Kholumolumo, formerly "Kholumolumosaurus" or "Thotobolosaurus", is an extinct genus of massopodan sauropodomorph dinosaur, which was closely related to Sarahsaurus, from the lower Elliot Formation of Maphutseng, Lesotho. The type species, Kholumolumo ellenbergerorum was formally described in 2020.
The Brandwater Basin is the drainage basin of the Brandwater River, a tributary of the Grootspruit River in the south-east of Orange Free State, South Africa, north of Lesotho. The basin is situated south of Bethlehem and south-east of Senekal, between the Witteberg to the west and north, the Rooiberge to the east, and the Drakensberg over the Caledon River to the south. It is also northwest of the Slaapkrans Basin and the Maloti Mountains on the northern border of Lesotho. Towns in the Brandwater Basin are Fouriesburg, founded in 1892, and Clarens, established in 1912.
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