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Three Rondavels - Sunset
Three Rondavels - Sonnenuntergang
The Blyde River Canyon, officially the Motlatse Canyon is a significant natural feature of South Africa, located in Mpumalanga, and forming the northern part of the Drakensberg escarpment. Located in the Blyde River Canyon Nature Reserve, it is 25 kilometres (16 mi) in length and is, on average, around 750 metres (2,461 ft) deep. The Blyderivierpoort Dam, when full, is at an altitude of 665 metres (2,182 ft). The canyon consists mostly of red sandstone. The highest point of the canyon, Mariepskop, is 1,944 metres (6,378 ft) above sea level, whilst its lowest point where the river leaves the canyon is slightly less than 561 metres (1,841 ft) above sea level. This means that by some measure the canyon is 1,383 metres (4,537 ft) deep.
While it is difficult to compare canyons world-wide, Blyde River Canyon is one of the largest canyons on Earth, and it may be the largest 'green canyon' due to its lush subtropical foliage. It has some of the deepest precipitous cliffs of any canyon on the planet. It is the second largest canyon in Africa, after the Fish River Canyon, and is known as one of the great wonders of nature on the continent.
Possibly the best view in the whole of the Blyde River Canyon is of the "Three Rondavels", huge, round rocks, thought to be reminiscent of the houses or huts of the indigenous people, known as rondavels. This canyon is part of the Panorama Route. This route starts at the town Graskop and includes God's Window, the Pinnacle and Bourke's Luck Potholes.
Blyde means "glad" or "happy" in old Dutch, a name derived from a voortrekkers' expedition. The 'happy river' was thus named in 1844, when Hendrik Potgieter and others returned safely from Delagoa Bay to the rest of their party of trekkers who had considered them dead. While still under this misapprehension they had named the nearby river where they had been encamped, Treurrivier, or 'mourning river'.
In 2005, the Blyde River was renamed to the Motlatse River, and the Mpumalanga Provincial Government announced that the canyon would be renamed as well.
The Blyde River Canyon supports large diversity of life, including numerous fish and antelope species as well as hippos and crocodiles, and every primate species that may be seen in South Africa (including both greater and lesser bushbabies, vervet monkeys and Samango monkeys). The diversity of birdlife is similarly high, including the beautiful and much sought Narina trogon as well as species such as the Cape vulture, black eagle, crowned eagle, African fish eagle, gymnogene, jackal buzzard, white-rumped vulture, bald ibis, African finfoot, Knysna lourie, purple-crested lourie, Gurney's sugarbird, malachite sunbird, cinnamon dove, African emerald cuckoo, red-backed mannikin, golden-tailed woodpecker, olive bush shrike, green twinspot, Taita falcons (very rarely sighted, a breeding pair lives in the nearby Abel Erasmus Pass), Cape eagle owl, white-faced owl, wood owl, peregrine falcon, black-breasted snake eagle, Wahlberg's eagle, long-crested eagle, lanner falcon, red-breasted sparrowhawk, rock kestrel and others.
At 200 metres (660 ft), the Kadishi Tufa waterfall is the second tallest tufa waterfall on earth. A tufa waterfall is formed when water running over dolomite rock absorbs calcium, and deposits rock formations more rapidly than they erode the surrounding rock. In the case of the Kadishi Tufa fall, the formation that has been produced strikingly resembles a face which is crying profusely, and is thus sometimes known as 'the weeping face of nature'.
The canyon and the surrounding Drakensberg escarpment is a very popular tourist region with a well-developed tourism industry supported by good public infrastructure.
(Wikipedia)
The Three Rondavels are three round, grass-covered mountain tops with somewhat pointed peaks. They resemble the traditional round or oval rondavels or African homesteads quite closely, which are made with local materials. Sometimes they are also called the Three Sisters, though this may confuse them with a similar threesome visible from the N1 road in the Northern Cape, very far to the south.
The names of the peaks commemorate a 19th century chief, Maripi, and three of his wives. The flat-topped peak adjacent to the rondavels is Mapjaneng, "the chief", who is remembered for opposing invading Swazis in a memorable battle. The three rondavels are named for three of his more troublesome wives – Magabolle, Mogoladikwe and Maseroto. Behind the rondavels the distant high plateau of Mariepskop may be visible. Beside the dam, the isolated Thabaneng hill is known as the "sundial" or “mountain with a shadow that moves". It is said that the position of its shadow indicates the time of day.
On a clear day the lookout point provides extensive views. From here one looks over the canyon to the Three Rondavels on the other side, which is flanked on various sides by promontories of the northern Drakensberg range.
The formation of the attractive sedimentary formations are explained geologically as the slow erosion of underlying soft stone, leaving the exposed the more resistant quartzite and shale rondavels.
(Wikipedia)
Der Blyde River Canyon ist ein 26 Kilometer langer, bis 800 Meter tiefer und hauptsächlich aus rotem Sandstein bestehender Canyon. Er befindet sich an der Panorama Route nordöstlich von Johannesburg und gilt als eines der großen Naturwunder Afrikas.
Durch den Blyde River Canyon, der an den Bourke’s Luck Potholes beginnt, fließt der Fluss Blyde River, der bei 25° 4′ 15,9″ S, 30° 40′ 40,2″ O dem Thaba Chweu entspringt und bei 24° 15′ 18,6″ S, 30° 49′ 50″ O in den Olifantsriver fließt.
Ein von zahlreichen Touristen besuchter Punkt des Canyons sind die drei Rondavels, gewaltige, runde Felsen, die an die runden Hütten der Einheimischen erinnern. Wegen seines Ausblicks vielbesucht ist auch God’s Window.
(Wikipedia)
Oribi Loop Road
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 paleontology finds have been made in the park, including dinosaur eggs and skeletons.
"Golden Gate" refers to the sandstone cliffs found on either side of the valley at the Golden Gate dam. In 1875, a farmer called J.N.R. van Reenen and his wife stopped here as they travelled to their new farm in Vuurland. He named the location "Golden Gate" when he saw the last rays of the setting sun fall on the cliffs.
In 1963, 47.92 km2 (11,840 acres) were proclaimed as a national park, specifically to preserve the scenic beauty of the area. In 1981, the park was enlarged to 62.41 km2 (15,420 acres), and in 1988, it was enlarged to 116.33 km2 (28,750 acres). In 2004, the park was announced to be joining with the neighbouring QwaQwa National Park. The amalgamation of QwaQwa National Park was completed in 2007, increasing the park's area to 340 km2 (84,000 acres).
The park is 320 km (200 mi) from Johannesburg and is close to the villages of Clarens and Kestell, in the upper regions of the Little Caledon River. The park is situated in the Rooiberge of the eastern Free State, in the foothills of the Maluti Mountains. The Caledon River forms the southern boundary of the park, as well as the border between the Free State and Lesotho. The highest peak in the park (and also in the Free State) is Ribbokkop at 2,829 m (9,281 ft) above sea level.
The park is located in the eastern highveld region of South Africa, and experiences a dry, sunny climate from June to August. It has showers, hail, and thunderstorms between October and April. It has thick snowfalls in the winter. The park has a relatively high rainfall of 800 mm (31 in) per year.
The park is an area of rich highveld and montane grassland flora. It has more than 60 grass species and a large variety of bulbs and herbs. Each of these species has its own flowering time, meaning that veld flowers can be seen throughout the summer. The park also has Afromontane forests and high-altitude Austro-Afro alpine grassland, which is scarce in South Africa. The ouhout (Leucosidea sericea), an evergreen species, is the most common tree in the park. Ouhout is a favourite habitat of beetles and 117 species occur on these trees in the park. The Lombardi poplars and weeping willows in the park are introduced species, but are kept because of their cultural and historic connection with the eastern Free State. Other exotic species in the park, for example wattle and bluegum, are systematically eradicated.
Instead of reintroducing one of the "big five" into the park, the sungazer lizard and water mongoose were reintroduced. Twelve species of mice, 10 species of carnivores, and 10 antelope species have been recorded in the park. The grey rhebuck and the mountain reedbuck were present when the park was established.
The geology of the park provides very visual "textbook" examples of Southern Africa's geological history. The sandstone formations in the park form the upper part of the Karoo Supergroup. These formations were deposited during a period of aeolian deposition towards the end of the Triassic Period. At the time of deposition, the climate of the area the park covers was becoming progressively drier until arid desert conditions set in, resulting in a land of dunes and sandy desert, with occasional scattered oases. The deposition of the sandstones ended when lava flowed out over the desert 190 million years ago.
The following sequence of geological formations is visible in the park (starting from the bottom): the Molteno Formation, Elliott Formation, Clarens Formation, and Drakensberg Formation. The yellow-brown Golden Gate and Brandwag cliffs are made up of the Clarens formation. The layers in this formation are 140 to 160 m (460 to 520 ft) thick. The Drakensberg formation comprises the basaltic lava that flowed over the desert. It forms the mountain summits in the park. On Ribbokkop, it is 600 m (2,000 ft) thick. The Elliot Formation is a red mudstone where many dinosaur fossils have been found.
The oldest dinosaur embryos ever discovered were found in the park in 1978. The eggs were from the Triassic Period (220 to 195 million years ago) and had fossilised foetal skeletons of Massospondylus, a prosauropod dinosaur. More examples of these eggs have since been found in the park. Other fossils found in the park include those of advanced cynodontia (canine toothed animals), small thecodontia (animals with teeth set firmly in the jaw), and bird-like and crocodile-like dinosaurs.
Accommodation in the park is available at Glen Reenen and Brandwag Rest camps. Caravan and camp sites with all amenities are available at Glen Reenen camp. The hotel was formerly part of Brandwag camp, but since its recent refurbishment, it is managed separately by SANParks as Golden Gate Hotel. The nearest town to Golden Gate Highlands National Park is Clarens (17 km to the west), but Phuthaditjhaba is also easily reached by a good tar road, driving through the access gate to the east of the park.
This park will be included into the Maloti-Drakensberg Transfrontier Conservation Area, Peace Park.
(Wikipedia)
Der Golden-Gate-Highlands-Nationalpark (englisch Golden Gate Highlands National Park) liegt in Südafrika, im Südosten des Freistaates nahe der Grenze zu Lesotho, und zeichnet sich besonders durch seine malerischen Felslandschaften aus. Orange oder ocker gefärbte Sandsteinfelsen ragen über das bergige Grasland auf. Außerdem gibt es Felsmalereien der San.
Der nördliche Eingang zum Park liegt bei dem Künstlerdorf Clarens.
(Wikipedia)
Sunrise seen from Highlands Mountain Retreat.
Sonnenaufgang vom Highlands Mountain Retreat gesehen.
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 paleontology finds have been made in the park, including dinosaur eggs and skeletons.
"Golden Gate" refers to the sandstone cliffs found on either side of the valley at the Golden Gate dam. In 1875, a farmer called J.N.R. van Reenen and his wife stopped here as they travelled to their new farm in Vuurland. He named the location "Golden Gate" when he saw the last rays of the setting sun fall on the cliffs.
In 1963, 47.92 km2 (11,840 acres) were proclaimed as a national park, specifically to preserve the scenic beauty of the area. In 1981, the park was enlarged to 62.41 km2 (15,420 acres), and in 1988, it was enlarged to 116.33 km2 (28,750 acres). In 2004, the park was announced to be joining with the neighbouring QwaQwa National Park. The amalgamation of QwaQwa National Park was completed in 2007, increasing the park's area to 340 km2 (84,000 acres).
The park is 320 km (200 mi) from Johannesburg and is close to the villages of Clarens and Kestell, in the upper regions of the Little Caledon River. The park is situated in the Rooiberge of the eastern Free State, in the foothills of the Maluti Mountains. The Caledon River forms the southern boundary of the park, as well as the border between the Free State and Lesotho. The highest peak in the park (and also in the Free State) is Ribbokkop at 2,829 m (9,281 ft) above sea level.
The park is located in the eastern highveld region of South Africa, and experiences a dry, sunny climate from June to August. It has showers, hail, and thunderstorms between October and April. It has thick snowfalls in the winter. The park has a relatively high rainfall of 800 mm (31 in) per year.
The park is an area of rich highveld and montane grassland flora. It has more than 60 grass species and a large variety of bulbs and herbs. Each of these species has its own flowering time, meaning that veld flowers can be seen throughout the summer. The park also has Afromontane forests and high-altitude Austro-Afro alpine grassland, which is scarce in South Africa. The ouhout (Leucosidea sericea), an evergreen species, is the most common tree in the park. Ouhout is a favourite habitat of beetles and 117 species occur on these trees in the park. The Lombardi poplars and weeping willows in the park are introduced species, but are kept because of their cultural and historic connection with the eastern Free State. Other exotic species in the park, for example wattle and bluegum, are systematically eradicated.
Instead of reintroducing one of the "big five" into the park, the sungazer lizard and water mongoose were reintroduced. Twelve species of mice, 10 species of carnivores, and 10 antelope species have been recorded in the park. The grey rhebuck and the mountain reedbuck were present when the park was established.
The geology of the park provides very visual "textbook" examples of Southern Africa's geological history. The sandstone formations in the park form the upper part of the Karoo Supergroup. These formations were deposited during a period of aeolian deposition towards the end of the Triassic Period. At the time of deposition, the climate of the area the park covers was becoming progressively drier until arid desert conditions set in, resulting in a land of dunes and sandy desert, with occasional scattered oases. The deposition of the sandstones ended when lava flowed out over the desert 190 million years ago.
The following sequence of geological formations is visible in the park (starting from the bottom): the Molteno Formation, Elliott Formation, Clarens Formation, and Drakensberg Formation. The yellow-brown Golden Gate and Brandwag cliffs are made up of the Clarens formation. The layers in this formation are 140 to 160 m (460 to 520 ft) thick. The Drakensberg formation comprises the basaltic lava that flowed over the desert. It forms the mountain summits in the park. On Ribbokkop, it is 600 m (2,000 ft) thick. The Elliot Formation is a red mudstone where many dinosaur fossils have been found.
The oldest dinosaur embryos ever discovered were found in the park in 1978. The eggs were from the Triassic Period (220 to 195 million years ago) and had fossilised foetal skeletons of Massospondylus, a prosauropod dinosaur. More examples of these eggs have since been found in the park. Other fossils found in the park include those of advanced cynodontia (canine toothed animals), small thecodontia (animals with teeth set firmly in the jaw), and bird-like and crocodile-like dinosaurs.
Accommodation in the park is available at Glen Reenen and Brandwag Rest camps. Caravan and camp sites with all amenities are available at Glen Reenen camp. The hotel was formerly part of Brandwag camp, but since its recent refurbishment, it is managed separately by SANParks as Golden Gate Hotel. The nearest town to Golden Gate Highlands National Park is Clarens (17 km to the west), but Phuthaditjhaba is also easily reached by a good tar road, driving through the access gate to the east of the park.
This park will be included into the Maloti-Drakensberg Transfrontier Conservation Area, Peace Park.
(Wikipedia)
Der Golden-Gate-Highlands-Nationalpark (englisch Golden Gate Highlands National Park) liegt in Südafrika, im Südosten des Freistaates nahe der Grenze zu Lesotho, und zeichnet sich besonders durch seine malerischen Felslandschaften aus. Orange oder ocker gefärbte Sandsteinfelsen ragen über das bergige Grasland auf. Außerdem gibt es Felsmalereien der San.
Der nördliche Eingang zum Park liegt bei dem Künstlerdorf Clarens.
(Wikipedia)
Berlin skyline in the dusk during total lunar eclipse July 27,2018.
Berlin in der Dämmerung.
27.7.2018, am Abend der Mondfinsternis.
Funkturm, Fernsehturm, Dom, Rotes Rathaus.
Blick vom Drachenberg
Sunset
Sonnenuntergang
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 paleontology finds have been made in the park, including dinosaur eggs and skeletons.
"Golden Gate" refers to the sandstone cliffs found on either side of the valley at the Golden Gate dam. In 1875, a farmer called J.N.R. van Reenen and his wife stopped here as they travelled to their new farm in Vuurland. He named the location "Golden Gate" when he saw the last rays of the setting sun fall on the cliffs.
In 1963, 47.92 km2 (11,840 acres) were proclaimed as a national park, specifically to preserve the scenic beauty of the area. In 1981, the park was enlarged to 62.41 km2 (15,420 acres), and in 1988, it was enlarged to 116.33 km2 (28,750 acres). In 2004, the park was announced to be joining with the neighbouring QwaQwa National Park. The amalgamation of QwaQwa National Park was completed in 2007, increasing the park's area to 340 km2 (84,000 acres).
The park is 320 km (200 mi) from Johannesburg and is close to the villages of Clarens and Kestell, in the upper regions of the Little Caledon River. The park is situated in the Rooiberge of the eastern Free State, in the foothills of the Maluti Mountains. The Caledon River forms the southern boundary of the park, as well as the border between the Free State and Lesotho. The highest peak in the park (and also in the Free State) is Ribbokkop at 2,829 m (9,281 ft) above sea level.
The park is located in the eastern highveld region of South Africa, and experiences a dry, sunny climate from June to August. It has showers, hail, and thunderstorms between October and April. It has thick snowfalls in the winter. The park has a relatively high rainfall of 800 mm (31 in) per year.
The park is an area of rich highveld and montane grassland flora. It has more than 60 grass species and a large variety of bulbs and herbs. Each of these species has its own flowering time, meaning that veld flowers can be seen throughout the summer. The park also has Afromontane forests and high-altitude Austro-Afro alpine grassland, which is scarce in South Africa. The ouhout (Leucosidea sericea), an evergreen species, is the most common tree in the park. Ouhout is a favourite habitat of beetles and 117 species occur on these trees in the park. The Lombardi poplars and weeping willows in the park are introduced species, but are kept because of their cultural and historic connection with the eastern Free State. Other exotic species in the park, for example wattle and bluegum, are systematically eradicated.
Instead of reintroducing one of the "big five" into the park, the sungazer lizard and water mongoose were reintroduced. Twelve species of mice, 10 species of carnivores, and 10 antelope species have been recorded in the park. The grey rhebuck and the mountain reedbuck were present when the park was established.
The geology of the park provides very visual "textbook" examples of Southern Africa's geological history. The sandstone formations in the park form the upper part of the Karoo Supergroup. These formations were deposited during a period of aeolian deposition towards the end of the Triassic Period. At the time of deposition, the climate of the area the park covers was becoming progressively drier until arid desert conditions set in, resulting in a land of dunes and sandy desert, with occasional scattered oases. The deposition of the sandstones ended when lava flowed out over the desert 190 million years ago.
The following sequence of geological formations is visible in the park (starting from the bottom): the Molteno Formation, Elliott Formation, Clarens Formation, and Drakensberg Formation. The yellow-brown Golden Gate and Brandwag cliffs are made up of the Clarens formation. The layers in this formation are 140 to 160 m (460 to 520 ft) thick. The Drakensberg formation comprises the basaltic lava that flowed over the desert. It forms the mountain summits in the park. On Ribbokkop, it is 600 m (2,000 ft) thick. The Elliot Formation is a red mudstone where many dinosaur fossils have been found.
The oldest dinosaur embryos ever discovered were found in the park in 1978. The eggs were from the Triassic Period (220 to 195 million years ago) and had fossilised foetal skeletons of Massospondylus, a prosauropod dinosaur. More examples of these eggs have since been found in the park. Other fossils found in the park include those of advanced cynodontia (canine toothed animals), small thecodontia (animals with teeth set firmly in the jaw), and bird-like and crocodile-like dinosaurs.
Accommodation in the park is available at Glen Reenen and Brandwag Rest camps. Caravan and camp sites with all amenities are available at Glen Reenen camp. The hotel was formerly part of Brandwag camp, but since its recent refurbishment, it is managed separately by SANParks as Golden Gate Hotel. The nearest town to Golden Gate Highlands National Park is Clarens (17 km to the west), but Phuthaditjhaba is also easily reached by a good tar road, driving through the access gate to the east of the park.
This park will be included into the Maloti-Drakensberg Transfrontier Conservation Area, Peace Park.
(Wikipedia)
Der Golden-Gate-Highlands-Nationalpark (englisch Golden Gate Highlands National Park) liegt in Südafrika, im Südosten des Freistaates nahe der Grenze zu Lesotho, und zeichnet sich besonders durch seine malerischen Felslandschaften aus. Orange oder ocker gefärbte Sandsteinfelsen ragen über das bergige Grasland auf. Außerdem gibt es Felsmalereien der San.
Der nördliche Eingang zum Park liegt bei dem Künstlerdorf Clarens.
(Wikipedia)
Sunrise seen from Highlands Mountain Retreat.
Sonnenaufgang vom Highlands Mountain Retreat gesehen.
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 paleontology finds have been made in the park, including dinosaur eggs and skeletons.
"Golden Gate" refers to the sandstone cliffs found on either side of the valley at the Golden Gate dam. In 1875, a farmer called J.N.R. van Reenen and his wife stopped here as they travelled to their new farm in Vuurland. He named the location "Golden Gate" when he saw the last rays of the setting sun fall on the cliffs.
In 1963, 47.92 km2 (11,840 acres) were proclaimed as a national park, specifically to preserve the scenic beauty of the area. In 1981, the park was enlarged to 62.41 km2 (15,420 acres), and in 1988, it was enlarged to 116.33 km2 (28,750 acres). In 2004, the park was announced to be joining with the neighbouring QwaQwa National Park. The amalgamation of QwaQwa National Park was completed in 2007, increasing the park's area to 340 km2 (84,000 acres).
The park is 320 km (200 mi) from Johannesburg and is close to the villages of Clarens and Kestell, in the upper regions of the Little Caledon River. The park is situated in the Rooiberge of the eastern Free State, in the foothills of the Maluti Mountains. The Caledon River forms the southern boundary of the park, as well as the border between the Free State and Lesotho. The highest peak in the park (and also in the Free State) is Ribbokkop at 2,829 m (9,281 ft) above sea level.
The park is located in the eastern highveld region of South Africa, and experiences a dry, sunny climate from June to August. It has showers, hail, and thunderstorms between October and April. It has thick snowfalls in the winter. The park has a relatively high rainfall of 800 mm (31 in) per year.
The park is an area of rich highveld and montane grassland flora. It has more than 60 grass species and a large variety of bulbs and herbs. Each of these species has its own flowering time, meaning that veld flowers can be seen throughout the summer. The park also has Afromontane forests and high-altitude Austro-Afro alpine grassland, which is scarce in South Africa. The ouhout (Leucosidea sericea), an evergreen species, is the most common tree in the park. Ouhout is a favourite habitat of beetles and 117 species occur on these trees in the park. The Lombardi poplars and weeping willows in the park are introduced species, but are kept because of their cultural and historic connection with the eastern Free State. Other exotic species in the park, for example wattle and bluegum, are systematically eradicated.
Instead of reintroducing one of the "big five" into the park, the sungazer lizard and water mongoose were reintroduced. Twelve species of mice, 10 species of carnivores, and 10 antelope species have been recorded in the park. The grey rhebuck and the mountain reedbuck were present when the park was established.
The geology of the park provides very visual "textbook" examples of Southern Africa's geological history. The sandstone formations in the park form the upper part of the Karoo Supergroup. These formations were deposited during a period of aeolian deposition towards the end of the Triassic Period. At the time of deposition, the climate of the area the park covers was becoming progressively drier until arid desert conditions set in, resulting in a land of dunes and sandy desert, with occasional scattered oases. The deposition of the sandstones ended when lava flowed out over the desert 190 million years ago.
The following sequence of geological formations is visible in the park (starting from the bottom): the Molteno Formation, Elliott Formation, Clarens Formation, and Drakensberg Formation. The yellow-brown Golden Gate and Brandwag cliffs are made up of the Clarens formation. The layers in this formation are 140 to 160 m (460 to 520 ft) thick. The Drakensberg formation comprises the basaltic lava that flowed over the desert. It forms the mountain summits in the park. On Ribbokkop, it is 600 m (2,000 ft) thick. The Elliot Formation is a red mudstone where many dinosaur fossils have been found.
The oldest dinosaur embryos ever discovered were found in the park in 1978. The eggs were from the Triassic Period (220 to 195 million years ago) and had fossilised foetal skeletons of Massospondylus, a prosauropod dinosaur. More examples of these eggs have since been found in the park. Other fossils found in the park include those of advanced cynodontia (canine toothed animals), small thecodontia (animals with teeth set firmly in the jaw), and bird-like and crocodile-like dinosaurs.
Accommodation in the park is available at Glen Reenen and Brandwag Rest camps. Caravan and camp sites with all amenities are available at Glen Reenen camp. The hotel was formerly part of Brandwag camp, but since its recent refurbishment, it is managed separately by SANParks as Golden Gate Hotel. The nearest town to Golden Gate Highlands National Park is Clarens (17 km to the west), but Phuthaditjhaba is also easily reached by a good tar road, driving through the access gate to the east of the park.
This park will be included into the Maloti-Drakensberg Transfrontier Conservation Area, Peace Park.
(Wikipedia)
Der Golden-Gate-Highlands-Nationalpark (englisch Golden Gate Highlands National Park) liegt in Südafrika, im Südosten des Freistaates nahe der Grenze zu Lesotho, und zeichnet sich besonders durch seine malerischen Felslandschaften aus. Orange oder ocker gefärbte Sandsteinfelsen ragen über das bergige Grasland auf. Außerdem gibt es Felsmalereien der San.
Der nördliche Eingang zum Park liegt bei dem Künstlerdorf Clarens.
(Wikipedia)
Blesbok Loop Road before sunset
Die Blesbok Loop Straße vor Sonnenuntergang
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 paleontology finds have been made in the park, including dinosaur eggs and skeletons.
"Golden Gate" refers to the sandstone cliffs found on either side of the valley at the Golden Gate dam. In 1875, a farmer called J.N.R. van Reenen and his wife stopped here as they travelled to their new farm in Vuurland. He named the location "Golden Gate" when he saw the last rays of the setting sun fall on the cliffs.
In 1963, 47.92 km2 (11,840 acres) were proclaimed as a national park, specifically to preserve the scenic beauty of the area. In 1981, the park was enlarged to 62.41 km2 (15,420 acres), and in 1988, it was enlarged to 116.33 km2 (28,750 acres). In 2004, the park was announced to be joining with the neighbouring QwaQwa National Park. The amalgamation of QwaQwa National Park was completed in 2007, increasing the park's area to 340 km2 (84,000 acres).
The park is 320 km (200 mi) from Johannesburg and is close to the villages of Clarens and Kestell, in the upper regions of the Little Caledon River. The park is situated in the Rooiberge of the eastern Free State, in the foothills of the Maluti Mountains. The Caledon River forms the southern boundary of the park, as well as the border between the Free State and Lesotho. The highest peak in the park (and also in the Free State) is Ribbokkop at 2,829 m (9,281 ft) above sea level.
The park is located in the eastern highveld region of South Africa, and experiences a dry, sunny climate from June to August. It has showers, hail, and thunderstorms between October and April. It has thick snowfalls in the winter. The park has a relatively high rainfall of 800 mm (31 in) per year.
The park is an area of rich highveld and montane grassland flora. It has more than 60 grass species and a large variety of bulbs and herbs. Each of these species has its own flowering time, meaning that veld flowers can be seen throughout the summer. The park also has Afromontane forests and high-altitude Austro-Afro alpine grassland, which is scarce in South Africa. The ouhout (Leucosidea sericea), an evergreen species, is the most common tree in the park. Ouhout is a favourite habitat of beetles and 117 species occur on these trees in the park. The Lombardi poplars and weeping willows in the park are introduced species, but are kept because of their cultural and historic connection with the eastern Free State. Other exotic species in the park, for example wattle and bluegum, are systematically eradicated.
Instead of reintroducing one of the "big five" into the park, the sungazer lizard and water mongoose were reintroduced. Twelve species of mice, 10 species of carnivores, and 10 antelope species have been recorded in the park. The grey rhebuck and the mountain reedbuck were present when the park was established.
The geology of the park provides very visual "textbook" examples of Southern Africa's geological history. The sandstone formations in the park form the upper part of the Karoo Supergroup. These formations were deposited during a period of aeolian deposition towards the end of the Triassic Period. At the time of deposition, the climate of the area the park covers was becoming progressively drier until arid desert conditions set in, resulting in a land of dunes and sandy desert, with occasional scattered oases. The deposition of the sandstones ended when lava flowed out over the desert 190 million years ago.
The following sequence of geological formations is visible in the park (starting from the bottom): the Molteno Formation, Elliott Formation, Clarens Formation, and Drakensberg Formation. The yellow-brown Golden Gate and Brandwag cliffs are made up of the Clarens formation. The layers in this formation are 140 to 160 m (460 to 520 ft) thick. The Drakensberg formation comprises the basaltic lava that flowed over the desert. It forms the mountain summits in the park. On Ribbokkop, it is 600 m (2,000 ft) thick. The Elliot Formation is a red mudstone where many dinosaur fossils have been found.
The oldest dinosaur embryos ever discovered were found in the park in 1978. The eggs were from the Triassic Period (220 to 195 million years ago) and had fossilised foetal skeletons of Massospondylus, a prosauropod dinosaur. More examples of these eggs have since been found in the park. Other fossils found in the park include those of advanced cynodontia (canine toothed animals), small thecodontia (animals with teeth set firmly in the jaw), and bird-like and crocodile-like dinosaurs.
Accommodation in the park is available at Glen Reenen and Brandwag Rest camps. Caravan and camp sites with all amenities are available at Glen Reenen camp. The hotel was formerly part of Brandwag camp, but since its recent refurbishment, it is managed separately by SANParks as Golden Gate Hotel. The nearest town to Golden Gate Highlands National Park is Clarens (17 km to the west), but Phuthaditjhaba is also easily reached by a good tar road, driving through the access gate to the east of the park.
This park will be included into the Maloti-Drakensberg Transfrontier Conservation Area, Peace Park.
(Wikipedia)
Der Golden-Gate-Highlands-Nationalpark (englisch Golden Gate Highlands National Park) liegt in Südafrika, im Südosten des Freistaates nahe der Grenze zu Lesotho, und zeichnet sich besonders durch seine malerischen Felslandschaften aus. Orange oder ocker gefärbte Sandsteinfelsen ragen über das bergige Grasland auf. Außerdem gibt es Felsmalereien der San.
Der nördliche Eingang zum Park liegt bei dem Künstlerdorf Clarens.
(Wikipedia)
Thukela Gorge Hike
Wanderung in die Thukela Schlucht
The uKhahlamba-Drakensberg Park is in the KwaZulu-Natal province of South Africa, covering 2,428.13 km2 (938 sq mi) of area. The park includes Royal Natal National Park, a provincial park, and covers part of the Drakensberg, the highest mountain range in Southern Africa.
The park and the adjoining Sehlabathebe National Park in the Kingdom of Lesotho are part of the Maloti-Drakensberg Park, which was first declared a World Heritage Site on 30 November 2000. It is described by UNESCO as having "exceptional natural beauty in its soaring basaltic buttresses, incisive dramatic cutbacks, and golden sandstone ramparts... the site’s diversity of habitats protects a high level of endemic and globally threatened species, especially birds and plants... [and it] also contains many caves and rock-shelters with the largest and most concentrated group of paintings in Africa south of the Sahara".
Plans to boost tourism in the area include a long-awaited cable car project by the KZN Economic Development, Tourism and Environmental Affairs Department.
The Drakensberg mountain range is characterized by a high level of endemism of both invertebrates and vertebrates.
Most of the higher South African parts of the Drakensberg mountain range have been designated as game reserves or wilderness areas. The uKhahlamba-Drakensberg Park is also in the List of Wetlands of International Importance (under the Ramsar Convention). Adjacent to the park is the Cathkin Estates Conservation and Wildlife Sanctuary, which spans 1,044 ha (10 km2) of virgin grassland and represents the largest privately owned game park in the KwaZulu-Natal Drakensberg region.
(Wikipedia)
The Royal Natal National Park is in the KwaZulu Natal province of South Africa and forms part of the uKhahlamba Drakensberg Park World Heritage Site. Notwithstanding the name, it is actually not a South African National Park managed by the SANParks, but rather a Provincial Park managed by Ezemvelo KZN Wildlife. This park is now included into the Maloti-Drakensberg Transfrontier Conservation Area Peace Park.
The main features of the park are the Drakensberg Amphitheatre, a rock wall 5 kilometres (3.1 mi) long by up to 1,200 metres (3,900 ft) high, Mont-Aux-Sources peak where the Orange and Tugela rivers have their source, and the 948-metre (3,110 ft) Tugela Falls, the world's second-highest waterfall.
(Wikipedia)
Der uKhahlamba-Drakensberg Park (isiZulu uKhahlamba = „Barriere aus Speeren“) ist ein Nationalpark in den Drakensbergen in Südafrika. Im November 2000 wurde der Park in die UNESCO-Welterbe-Liste eingetragen. Der Park wird von der Provinzbehörde Ezemvelo KZN Wildlife verwaltet.
Der Park bedeckt eine Fläche von 2428 km². Er liegt in der Provinz KwaZulu-Natal und bildet einen 180 Kilometer langen und bis zu 20 Kilometer breiten Streifen entlang der Grenze zum Königreich Lesotho. Weitere Bestandteile des uKhahlamba-Drakensberg Park sind die getrennt liegenden Gebiete Royal-Natal-Nationalpark und Spioenkop Dam Nature Reserve weiter im Norden.
Der Park verfügt über hochaufragende Bergformationen und ist mit einem gut ausgebauten Netz von Wanderpfaden durchzogen. Basaltene, senkrecht aufragende Bergpfeiler, Bastionen aus goldbraunem Sandstein sowie skulpturierte Bögen, Höhlen, Säulen und Felswannen prägen das Landschaftsbild. Die Kette der Drakensberge im uKhahlamba-Drakensberg Park umfasst mehrere über 3000 Meter hohe Gipfel wie den Mafadi, den Giant’s Castle, den Cathedral Peak, den Monk’s Cowl, den Champagne Castle und den Njesuthi. Die Berghänge sind teilweise als Naturschutzgebiete ausgewiesen, in denen sich rund 30.000 Felsmalereien in etwa 600 Höhlen finden, die von San-Menschen über einen Zeitraum von 4000 Jahren erstellt wurden. In dieser Region entspringen die meisten großen Flüsse der Provinz KwaZulu-Natal. Sie bilden tiefe Schluchten und Täler. Einzige Straßenverbindung durch den Park nach Lesotho ist die Strecke über den Sanipass.
Es gibt eine Vielfalt endemischer Pflanzenarten, darunter Zuckerbüsche. Im Frühjahr übersäen in den Niederungen Teppiche von Wildblumen den Park, darunter Watsonia-Arten.
Zu den Vogelarten gehören Kapgeier (Gyps coprotheres) und Bartgeier (Gypaetus barbatus). Zahlreiche im Park beheimatete Wirbeltiere und Wirbellose sind endemisch. Weiterhin leben im Park Buschböcke, Ducker, Elenantilopen und Paviane.
1903 beschloss die Regierung der Kolonie Natal die Errichtung eines Naturschutzgebietes in den Drakensbergen. 1905 wurde eine klare Grenzziehung des Schutzbereichs proklamiert. 1916 wurde der Royal Natal National Park eingerichtet. Ab den 1950er Jahren wurden in den Drakensbergen diverse Naturschutzgebiete ausgewiesen, so 1951 das Kamberg Nature Reserve, 1953 das Nature Reserve de Lotheni und 1967 Vergelegen. Dabei wurde der Gewässerschutz vorangetrieben. 1973 kamen die Schutzgebiete Mdedelelo und Mkomazi hinzu.
Im Juni 2001 wurde des Maloti-Drakensberg Transfrontier Conservation Area (etwa: Maloti-Drakensberge-Grenzüberschreitendes-Erhaltungsgebiet) gegründet. Dieses verbindet den ukhahlamba-Drakensberg Park mit dem Sehlabathebe-Nationalpark in Lesotho. Ihm liegt der Anspruch an einen Peace Park (Transfrontier Conservation Area/TFCA) zugrunde. Die zwölf Kilometer lange Staatsgrenze kann zu Fuß passiert werden. Seit 2013 sind beide Nationalparks zusammen als Maloti Drakensberg Transboundary World Heritage Site in der UNESCO-Welterbe-Liste verzeichnet. Der gesamte Park ist nunmehr 2493 km² groß, wobei 65 km² der Fläche auf das Terrain Lesothos entfallen.
„… exceptional natural beauty in its soaring basaltic buttresses, incisive dramatic cutbacks, and golden sandstone ramparts … the site’s diversity of habitats protects a high level of endemic and globally threatened species, especially birds and plants … [and it] also contains many caves and rock-shelters with the largest and most concentrated group of paintings in Africa south of the Sahara. – … außergewöhnliche Schönheit der Natur in seinen aufragenden Basaltpfeilern, prägnante dramatische Einschnitte, und goldene Sandstein-Wälle … Die Vielfalt der Lebensräume beschützt ein hohes Maß an endemischen und vom Aussterben bedrohten Arten, vor allem Vögel und Pflanzen … [und es] enthält viele Höhlen und Felsnischen mit der größten und dichtesten Gruppe von Gemälden in Afrika südlich der Sahara.“
– Beschreibung des Maloti-Drakensberg Transfrontier Conservation Area auf der Website der UNESCO: Begründung zur Auswahl 2013
Teile der Drakensberg-Gebirgskette sind zu Schutzzwecken mit übergeordneter Bedeutung als Totalreservate ausgewiesen, sowie für touristische Zwecke daneben als Wildreservate. Entsprechend der Ramsar-Konvention wird der uKhahlamba Drakensberg Park auch als Schutzgut der List of Ramsar wetlands of international importance geführt. Private Eigentumsrechte hält an kleineren Gebietsteilen die Cathkin Estates Conservation and Wildlife Sanctuary.
(Wikipedia)
Der Royal Natal National Park wurde 1916 in den südafrikanischen Drakensbergen in der heutigen Provinz KwaZulu-Natal gebildet. Er ist Teil des Ukhahlamba-Drakensberg Park, der zum UNESCO-Welterbe gehört. Er gehört zu den spektakulärsten Natursehenswürdigkeiten in Afrika. Beeindruckend ist das Amphitheatre, eine mehrere Kilometer lange und etwa 1000 Meter hohe Felswand zwischen Sentinel (3165 m) und Eastern Buttress (3047 m). Auf dem flachen Gipfelplateau stehen einige Berge wie der Mont-Aux-Sources (Sesotho: Phofung) (3282 m), den 1836 die französischen Missionare Thomas Arbousset und François Daumas bestiegen und nach den Quellen von drei größeren Flüssen benannten.
Einer von diesen, der Tugela, stürzt in den Tugelafällen in fünf Stufen 948 Meter in die Tiefe (andere Angaben: knapp 3000 Fuß, 540 m). In kalten Wintern friert er in den oberen Stufen und bildet eindrucksvolle Eissäulen.
Der Royal Natal National Park ist ideal geeignet für Wanderungen mit einem Netz von klassifizierten Wegen aller Schwierigkeitsgrade; dies reicht von der leichten Besteigung des Mont-aux-Sources vom Plateau aus bis zur jährlichen Mont-aux-Sources Challenge, wenn Querfeldeinläufer zusammenkommen, um die 50 Kilometer lange Strecke in weniger als fünf Stunden zu absolvieren.
(Wikipedia)
Berlin Falls
The Panorama Route is a scenic road in South Africa connecting several cultural and natural points of interest. This route, steeped in the history of South Africa, is situated in the Mpumalanga province. The route is centred around the Blyde River Canyon, the world’s third largest canyon, and features numerous waterfalls, one of the largest afforested areas in South Africa, and several natural landmarks. The route starts at the foot of the Long Tom Pass just outside Lydenburg, following the natural descent from the Great Escarpment to the Lowveld, and ending at the border of the Mpumalanga and Limpopo provinces near the Echo Caves.
This route is deeply entrenched in the history of South Africa. From 1871, parts of the route were used as a transport road between Lydenburg and Delagoa Bay. It is also on this route that General Louis Botha fled from the English during the Anglo Boer War, and houses one of the most famous Victorian age canons in the world, “The Long Tom”.
Many towns on the route, such as Pilgrim’s Rest, were established during the Transvaal gold rush in the late 1800s. Thousands of fortune seekers crossed the treacherous mountains and rugged terrain in the search of gold. One of these was a former storekeeper from Pilgrim’s Rest, Percy Fitzpatrick. He wrote the popular book Jock of the Bushveld, recounting some of the adventures he shared with his faithful bull terrier Jock, whilst traversing this famous route.
(Wikipedia)
The Berlin Falls is a waterfall in Mpumalanga, South Africa. They are located close to God's Window and the highest waterfall in South Africa's Mpumalanga province, Lisbon Falls. Whilst less than a tenth of the heigh of South Africa's tallest waterfall, the Tugela Falls, they are nonetheless extremely beautiful. Berlin Falls, which forms part of the Blyde River Canyon on the Panorama route, is one of several waterfalls that can be found in the Sabie region – the others being Horseshoe Falls, Lone Creek Falls, Bridal Veil Falls, Mac-Mac Falls, and the highest waterfall in Mpumalanga, Lisbon Falls, which is a staggering 90m high.
The Berlin Falls cascade from the centre of a sheer cliff that stands roughly 80m tall. The shape of the falls is likened to a giant candle. A narrow, natural channel at the top of the falls creates the ‘wick’ of the candle, and as the water drops from this point, it fans out creating the rest of the candle before emptying out into the pool below.
Berlin Falls gets its name from miners who ventured to South Africa from Europe during the gold rush, and named each waterfall in the region after their home towns, or places from their home countries.
Visitors to the Berlin Falls can explore the area by foot, enjoy a picnic around the waterfall, and even take a dip in the pool at the base of the waterfall. Be sure to look out for the Blyde River Protea which is endemic to this area. Birding enthusiasts will also enjoy the numerous bird species which can be found in this region of the Mpumalanga escarpment. Binoculars and bird identification books are highly recommended.
The falls are on the Sabine River and fall 80 metres (260 ft), dumping into a circular basin flanked by red cliffs.
The falls have the shape of a candle, with the first short drop the wick, and the remaining, broader drop being the candle body.
The falls were named by German miners during the gold rush, who named locations after towns and places in their home country. Berlin Falls was named for the capital of Germany.
(Wikipedia)
Die Panorama Route (deutsch: Panoramastraße) ist eine Touristenattraktion in den Transvaal-Drakensbergen in der Provinz Mpumalanga im Osten Südafrikas. Sie ist wegen der steilen Abhänge mit Aussichten weit ins Flachland des Lowveld und interessanter Felsbildungen entlang der Straße eine Region mit touristisch bedeutsamen Sehenswürdigkeiten. Die als Panorama Route bezeichnete Streckenführung verläuft auf der Regionalstraße R532 und auf einem Teilstück der R37. Das Informationszentrum für Touristen befindet sich in dem Ort Graskop.
Entlang dem in Nord-Süd-Richtung verlaufenden Steilhang bricht das südafrikanische Hochland (Highveld) in das bis zu 1.000 Meter tiefer gelegene Flachland (Lowveld) ab, wo sich unter anderem der Kruger-Nationalpark befindet. Die Panorama Route bietet weite Ausblicke in die Ebene, beispielsweise bei God’s Window. Zu den bekannten Canyons entlang der Strecke gehört der Blyde River Canyon, der an den bizarren Erosionsformen der Bourke’s Luck Potholes seinen Ausgang nimmt.
Daneben entstanden durch Erosion zahlreiche Wasserfälle wie die Macmac Falls, Lisbon Falls und Berlin Falls.
Im Nahbereich der Panorama Route liegen auch die historische Goldgräberstadt Pilgrim’s Rest, die seit 1986 ein Nationaldenkmal ist, sowie die Sudwala Caves.
Der Steilhang ist durch dieselben geologischen Prozesse entstanden wie die gesamte Kette der Drakensberge. Zu einer starken Erosion führen die über das Lowveld aus Osten heranziehenden Regenwolken, die sich an dem Steilhang abregnen.
Neben dem Tourismus wird das Gebiet entlang der Panorama Route vorwiegend forstwirtschaftlich (Anbau von Nadelhölzern) genutzt. Daneben gibt es zahlreiche Farmen zur Fischzucht.
(Wikipedia)
Three Rondavels - Sunset
Three Rondavels - Sonnenuntergang
The Blyde River Canyon, officially the Motlatse Canyon is a significant natural feature of South Africa, located in Mpumalanga, and forming the northern part of the Drakensberg escarpment. Located in the Blyde River Canyon Nature Reserve, it is 25 kilometres (16 mi) in length and is, on average, around 750 metres (2,461 ft) deep. The Blyderivierpoort Dam, when full, is at an altitude of 665 metres (2,182 ft). The canyon consists mostly of red sandstone. The highest point of the canyon, Mariepskop, is 1,944 metres (6,378 ft) above sea level, whilst its lowest point where the river leaves the canyon is slightly less than 561 metres (1,841 ft) above sea level. This means that by some measure the canyon is 1,383 metres (4,537 ft) deep.
While it is difficult to compare canyons world-wide, Blyde River Canyon is one of the largest canyons on Earth, and it may be the largest 'green canyon' due to its lush subtropical foliage. It has some of the deepest precipitous cliffs of any canyon on the planet. It is the second largest canyon in Africa, after the Fish River Canyon, and is known as one of the great wonders of nature on the continent.
Possibly the best view in the whole of the Blyde River Canyon is of the "Three Rondavels", huge, round rocks, thought to be reminiscent of the houses or huts of the indigenous people, known as rondavels. This canyon is part of the Panorama Route. This route starts at the town Graskop and includes God's Window, the Pinnacle and Bourke's Luck Potholes.
Blyde means "glad" or "happy" in old Dutch, a name derived from a voortrekkers' expedition. The 'happy river' was thus named in 1844, when Hendrik Potgieter and others returned safely from Delagoa Bay to the rest of their party of trekkers who had considered them dead. While still under this misapprehension they had named the nearby river where they had been encamped, Treurrivier, or 'mourning river'.
In 2005, the Blyde River was renamed to the Motlatse River, and the Mpumalanga Provincial Government announced that the canyon would be renamed as well.
The Blyde River Canyon supports large diversity of life, including numerous fish and antelope species as well as hippos and crocodiles, and every primate species that may be seen in South Africa (including both greater and lesser bushbabies, vervet monkeys and Samango monkeys). The diversity of birdlife is similarly high, including the beautiful and much sought Narina trogon as well as species such as the Cape vulture, black eagle, crowned eagle, African fish eagle, gymnogene, jackal buzzard, white-rumped vulture, bald ibis, African finfoot, Knysna lourie, purple-crested lourie, Gurney's sugarbird, malachite sunbird, cinnamon dove, African emerald cuckoo, red-backed mannikin, golden-tailed woodpecker, olive bush shrike, green twinspot, Taita falcons (very rarely sighted, a breeding pair lives in the nearby Abel Erasmus Pass), Cape eagle owl, white-faced owl, wood owl, peregrine falcon, black-breasted snake eagle, Wahlberg's eagle, long-crested eagle, lanner falcon, red-breasted sparrowhawk, rock kestrel and others.
At 200 metres (660 ft), the Kadishi Tufa waterfall is the second tallest tufa waterfall on earth. A tufa waterfall is formed when water running over dolomite rock absorbs calcium, and deposits rock formations more rapidly than they erode the surrounding rock. In the case of the Kadishi Tufa fall, the formation that has been produced strikingly resembles a face which is crying profusely, and is thus sometimes known as 'the weeping face of nature'.
The canyon and the surrounding Drakensberg escarpment is a very popular tourist region with a well-developed tourism industry supported by good public infrastructure.
(Wikipedia)
The Three Rondavels are three round, grass-covered mountain tops with somewhat pointed peaks. They resemble the traditional round or oval rondavels or African homesteads quite closely, which are made with local materials. Sometimes they are also called the Three Sisters, though this may confuse them with a similar threesome visible from the N1 road in the Northern Cape, very far to the south.
The names of the peaks commemorate a 19th century chief, Maripi, and three of his wives. The flat-topped peak adjacent to the rondavels is Mapjaneng, "the chief", who is remembered for opposing invading Swazis in a memorable battle. The three rondavels are named for three of his more troublesome wives – Magabolle, Mogoladikwe and Maseroto. Behind the rondavels the distant high plateau of Mariepskop may be visible. Beside the dam, the isolated Thabaneng hill is known as the "sundial" or “mountain with a shadow that moves". It is said that the position of its shadow indicates the time of day.
On a clear day the lookout point provides extensive views. From here one looks over the canyon to the Three Rondavels on the other side, which is flanked on various sides by promontories of the northern Drakensberg range.
The formation of the attractive sedimentary formations are explained geologically as the slow erosion of underlying soft stone, leaving the exposed the more resistant quartzite and shale rondavels.
(Wikipedia)
Der Blyde River Canyon ist ein 26 Kilometer langer, bis 800 Meter tiefer und hauptsächlich aus rotem Sandstein bestehender Canyon. Er befindet sich an der Panorama Route nordöstlich von Johannesburg und gilt als eines der großen Naturwunder Afrikas.
Durch den Blyde River Canyon, der an den Bourke’s Luck Potholes beginnt, fließt der Fluss Blyde River, der bei 25° 4′ 15,9″ S, 30° 40′ 40,2″ O dem Thaba Chweu entspringt und bei 24° 15′ 18,6″ S, 30° 49′ 50″ O in den Olifantsriver fließt.
Ein von zahlreichen Touristen besuchter Punkt des Canyons sind die drei Rondavels, gewaltige, runde Felsen, die an die runden Hütten der Einheimischen erinnern. Wegen seines Ausblicks vielbesucht ist auch God’s Window.
(Wikipedia)
Hike around Plowman's Kop via the Crack and Mudslide.
Wanderung über den Plowman's Kop über Crack und Mudslide.
The uKhahlamba-Drakensberg Park is in the KwaZulu-Natal province of South Africa, covering 2,428.13 km2 (938 sq mi) of area. The park includes Royal Natal National Park, a provincial park, and covers part of the Drakensberg, the highest mountain range in Southern Africa.
The park and the adjoining Sehlabathebe National Park in the Kingdom of Lesotho are part of the Maloti-Drakensberg Park, which was first declared a World Heritage Site on 30 November 2000. It is described by UNESCO as having "exceptional natural beauty in its soaring basaltic buttresses, incisive dramatic cutbacks, and golden sandstone ramparts... the site’s diversity of habitats protects a high level of endemic and globally threatened species, especially birds and plants... [and it] also contains many caves and rock-shelters with the largest and most concentrated group of paintings in Africa south of the Sahara".
Plans to boost tourism in the area include a long-awaited cable car project by the KZN Economic Development, Tourism and Environmental Affairs Department.
The Drakensberg mountain range is characterized by a high level of endemism of both invertebrates and vertebrates.
Most of the higher South African parts of the Drakensberg mountain range have been designated as game reserves or wilderness areas. The uKhahlamba-Drakensberg Park is also in the List of Wetlands of International Importance (under the Ramsar Convention). Adjacent to the park is the Cathkin Estates Conservation and Wildlife Sanctuary, which spans 1,044 ha (10 km2) of virgin grassland and represents the largest privately owned game park in the KwaZulu-Natal Drakensberg region.
(Wikipedia)
The Royal Natal National Park is in the KwaZulu Natal province of South Africa and forms part of the uKhahlamba Drakensberg Park World Heritage Site. Notwithstanding the name, it is actually not a South African National Park managed by the SANParks, but rather a Provincial Park managed by Ezemvelo KZN Wildlife. This park is now included into the Maloti-Drakensberg Transfrontier Conservation Area Peace Park.
The main features of the park are the Drakensberg Amphitheatre, a rock wall 5 kilometres (3.1 mi) long by up to 1,200 metres (3,900 ft) high, Mont-Aux-Sources peak where the Orange and Tugela rivers have their source, and the 948-metre (3,110 ft) Tugela Falls, the world's second-highest waterfall.
(Wikipedia)
Der uKhahlamba-Drakensberg Park (isiZulu uKhahlamba = „Barriere aus Speeren“) ist ein Nationalpark in den Drakensbergen in Südafrika. Im November 2000 wurde der Park in die UNESCO-Welterbe-Liste eingetragen. Der Park wird von der Provinzbehörde Ezemvelo KZN Wildlife verwaltet.
Der Park bedeckt eine Fläche von 2428 km². Er liegt in der Provinz KwaZulu-Natal und bildet einen 180 Kilometer langen und bis zu 20 Kilometer breiten Streifen entlang der Grenze zum Königreich Lesotho. Weitere Bestandteile des uKhahlamba-Drakensberg Park sind die getrennt liegenden Gebiete Royal-Natal-Nationalpark und Spioenkop Dam Nature Reserve weiter im Norden.
Der Park verfügt über hochaufragende Bergformationen und ist mit einem gut ausgebauten Netz von Wanderpfaden durchzogen. Basaltene, senkrecht aufragende Bergpfeiler, Bastionen aus goldbraunem Sandstein sowie skulpturierte Bögen, Höhlen, Säulen und Felswannen prägen das Landschaftsbild. Die Kette der Drakensberge im uKhahlamba-Drakensberg Park umfasst mehrere über 3000 Meter hohe Gipfel wie den Mafadi, den Giant’s Castle, den Cathedral Peak, den Monk’s Cowl, den Champagne Castle und den Njesuthi. Die Berghänge sind teilweise als Naturschutzgebiete ausgewiesen, in denen sich rund 30.000 Felsmalereien in etwa 600 Höhlen finden, die von San-Menschen über einen Zeitraum von 4000 Jahren erstellt wurden. In dieser Region entspringen die meisten großen Flüsse der Provinz KwaZulu-Natal. Sie bilden tiefe Schluchten und Täler. Einzige Straßenverbindung durch den Park nach Lesotho ist die Strecke über den Sanipass.
Es gibt eine Vielfalt endemischer Pflanzenarten, darunter Zuckerbüsche. Im Frühjahr übersäen in den Niederungen Teppiche von Wildblumen den Park, darunter Watsonia-Arten.
Zu den Vogelarten gehören Kapgeier (Gyps coprotheres) und Bartgeier (Gypaetus barbatus). Zahlreiche im Park beheimatete Wirbeltiere und Wirbellose sind endemisch. Weiterhin leben im Park Buschböcke, Ducker, Elenantilopen und Paviane.
1903 beschloss die Regierung der Kolonie Natal die Errichtung eines Naturschutzgebietes in den Drakensbergen. 1905 wurde eine klare Grenzziehung des Schutzbereichs proklamiert. 1916 wurde der Royal Natal National Park eingerichtet. Ab den 1950er Jahren wurden in den Drakensbergen diverse Naturschutzgebiete ausgewiesen, so 1951 das Kamberg Nature Reserve, 1953 das Nature Reserve de Lotheni und 1967 Vergelegen. Dabei wurde der Gewässerschutz vorangetrieben. 1973 kamen die Schutzgebiete Mdedelelo und Mkomazi hinzu.
Im Juni 2001 wurde des Maloti-Drakensberg Transfrontier Conservation Area (etwa: Maloti-Drakensberge-Grenzüberschreitendes-Erhaltungsgebiet) gegründet. Dieses verbindet den ukhahlamba-Drakensberg Park mit dem Sehlabathebe-Nationalpark in Lesotho. Ihm liegt der Anspruch an einen Peace Park (Transfrontier Conservation Area/TFCA) zugrunde. Die zwölf Kilometer lange Staatsgrenze kann zu Fuß passiert werden. Seit 2013 sind beide Nationalparks zusammen als Maloti Drakensberg Transboundary World Heritage Site in der UNESCO-Welterbe-Liste verzeichnet. Der gesamte Park ist nunmehr 2493 km² groß, wobei 65 km² der Fläche auf das Terrain Lesothos entfallen.
„… exceptional natural beauty in its soaring basaltic buttresses, incisive dramatic cutbacks, and golden sandstone ramparts … the site’s diversity of habitats protects a high level of endemic and globally threatened species, especially birds and plants … [and it] also contains many caves and rock-shelters with the largest and most concentrated group of paintings in Africa south of the Sahara. – … außergewöhnliche Schönheit der Natur in seinen aufragenden Basaltpfeilern, prägnante dramatische Einschnitte, und goldene Sandstein-Wälle … Die Vielfalt der Lebensräume beschützt ein hohes Maß an endemischen und vom Aussterben bedrohten Arten, vor allem Vögel und Pflanzen … [und es] enthält viele Höhlen und Felsnischen mit der größten und dichtesten Gruppe von Gemälden in Afrika südlich der Sahara.“
– Beschreibung des Maloti-Drakensberg Transfrontier Conservation Area auf der Website der UNESCO: Begründung zur Auswahl 2013
Teile der Drakensberg-Gebirgskette sind zu Schutzzwecken mit übergeordneter Bedeutung als Totalreservate ausgewiesen, sowie für touristische Zwecke daneben als Wildreservate. Entsprechend der Ramsar-Konvention wird der uKhahlamba Drakensberg Park auch als Schutzgut der List of Ramsar wetlands of international importance geführt. Private Eigentumsrechte hält an kleineren Gebietsteilen die Cathkin Estates Conservation and Wildlife Sanctuary.
(Wikipedia)
Der Royal Natal National Park wurde 1916 in den südafrikanischen Drakensbergen in der heutigen Provinz KwaZulu-Natal gebildet. Er ist Teil des Ukhahlamba-Drakensberg Park, der zum UNESCO-Welterbe gehört. Er gehört zu den spektakulärsten Natursehenswürdigkeiten in Afrika. Beeindruckend ist das Amphitheatre, eine mehrere Kilometer lange und etwa 1000 Meter hohe Felswand zwischen Sentinel (3165 m) und Eastern Buttress (3047 m). Auf dem flachen Gipfelplateau stehen einige Berge wie der Mont-Aux-Sources (Sesotho: Phofung) (3282 m), den 1836 die französischen Missionare Thomas Arbousset und François Daumas bestiegen und nach den Quellen von drei größeren Flüssen benannten.
Einer von diesen, der Tugela, stürzt in den Tugelafällen in fünf Stufen 948 Meter in die Tiefe (andere Angaben: knapp 3000 Fuß, 540 m). In kalten Wintern friert er in den oberen Stufen und bildet eindrucksvolle Eissäulen.
Der Royal Natal National Park ist ideal geeignet für Wanderungen mit einem Netz von klassifizierten Wegen aller Schwierigkeitsgrade; dies reicht von der leichten Besteigung des Mont-aux-Sources vom Plateau aus bis zur jährlichen Mont-aux-Sources Challenge, wenn Querfeldeinläufer zusammenkommen, um die 50 Kilometer lange Strecke in weniger als fünf Stunden zu absolvieren.
(Wikipedia)
Hike around Plowman's Kop via the Crack and Mudslide
Wanderung über den Plowman's Kop über Crack und Mudslide
The uKhahlamba-Drakensberg Park is in the KwaZulu-Natal province of South Africa, covering 2,428.13 km2 (938 sq mi) of area. The park includes Royal Natal National Park, a provincial park, and covers part of the Drakensberg, the highest mountain range in Southern Africa.
The park and the adjoining Sehlabathebe National Park in the Kingdom of Lesotho are part of the Maloti-Drakensberg Park, which was first declared a World Heritage Site on 30 November 2000. It is described by UNESCO as having "exceptional natural beauty in its soaring basaltic buttresses, incisive dramatic cutbacks, and golden sandstone ramparts... the site’s diversity of habitats protects a high level of endemic and globally threatened species, especially birds and plants... [and it] also contains many caves and rock-shelters with the largest and most concentrated group of paintings in Africa south of the Sahara".
Plans to boost tourism in the area include a long-awaited cable car project by the KZN Economic Development, Tourism and Environmental Affairs Department.
The Drakensberg mountain range is characterized by a high level of endemism of both invertebrates and vertebrates.
Most of the higher South African parts of the Drakensberg mountain range have been designated as game reserves or wilderness areas. The uKhahlamba-Drakensberg Park is also in the List of Wetlands of International Importance (under the Ramsar Convention). Adjacent to the park is the Cathkin Estates Conservation and Wildlife Sanctuary, which spans 1,044 ha (10 km2) of virgin grassland and represents the largest privately owned game park in the KwaZulu-Natal Drakensberg region.
(Wikipedia)
The Royal Natal National Park is in the KwaZulu Natal province of South Africa and forms part of the uKhahlamba Drakensberg Park World Heritage Site. Notwithstanding the name, it is actually not a South African National Park managed by the SANParks, but rather a Provincial Park managed by Ezemvelo KZN Wildlife. This park is now included into the Maloti-Drakensberg Transfrontier Conservation Area Peace Park.
The main features of the park are the Drakensberg Amphitheatre, a rock wall 5 kilometres (3.1 mi) long by up to 1,200 metres (3,900 ft) high, Mont-Aux-Sources peak where the Orange and Tugela rivers have their source, and the 948-metre (3,110 ft) Tugela Falls, the world's second-highest waterfall.
(Wikipedia)
Der uKhahlamba-Drakensberg Park (isiZulu uKhahlamba = „Barriere aus Speeren“) ist ein Nationalpark in den Drakensbergen in Südafrika. Im November 2000 wurde der Park in die UNESCO-Welterbe-Liste eingetragen. Der Park wird von der Provinzbehörde Ezemvelo KZN Wildlife verwaltet.
Der Park bedeckt eine Fläche von 2428 km². Er liegt in der Provinz KwaZulu-Natal und bildet einen 180 Kilometer langen und bis zu 20 Kilometer breiten Streifen entlang der Grenze zum Königreich Lesotho. Weitere Bestandteile des uKhahlamba-Drakensberg Park sind die getrennt liegenden Gebiete Royal-Natal-Nationalpark und Spioenkop Dam Nature Reserve weiter im Norden.
Der Park verfügt über hochaufragende Bergformationen und ist mit einem gut ausgebauten Netz von Wanderpfaden durchzogen. Basaltene, senkrecht aufragende Bergpfeiler, Bastionen aus goldbraunem Sandstein sowie skulpturierte Bögen, Höhlen, Säulen und Felswannen prägen das Landschaftsbild. Die Kette der Drakensberge im uKhahlamba-Drakensberg Park umfasst mehrere über 3000 Meter hohe Gipfel wie den Mafadi, den Giant’s Castle, den Cathedral Peak, den Monk’s Cowl, den Champagne Castle und den Njesuthi. Die Berghänge sind teilweise als Naturschutzgebiete ausgewiesen, in denen sich rund 30.000 Felsmalereien in etwa 600 Höhlen finden, die von San-Menschen über einen Zeitraum von 4000 Jahren erstellt wurden. In dieser Region entspringen die meisten großen Flüsse der Provinz KwaZulu-Natal. Sie bilden tiefe Schluchten und Täler. Einzige Straßenverbindung durch den Park nach Lesotho ist die Strecke über den Sanipass.
Es gibt eine Vielfalt endemischer Pflanzenarten, darunter Zuckerbüsche. Im Frühjahr übersäen in den Niederungen Teppiche von Wildblumen den Park, darunter Watsonia-Arten.
Zu den Vogelarten gehören Kapgeier (Gyps coprotheres) und Bartgeier (Gypaetus barbatus). Zahlreiche im Park beheimatete Wirbeltiere und Wirbellose sind endemisch. Weiterhin leben im Park Buschböcke, Ducker, Elenantilopen und Paviane.
1903 beschloss die Regierung der Kolonie Natal die Errichtung eines Naturschutzgebietes in den Drakensbergen. 1905 wurde eine klare Grenzziehung des Schutzbereichs proklamiert. 1916 wurde der Royal Natal National Park eingerichtet. Ab den 1950er Jahren wurden in den Drakensbergen diverse Naturschutzgebiete ausgewiesen, so 1951 das Kamberg Nature Reserve, 1953 das Nature Reserve de Lotheni und 1967 Vergelegen. Dabei wurde der Gewässerschutz vorangetrieben. 1973 kamen die Schutzgebiete Mdedelelo und Mkomazi hinzu.
Im Juni 2001 wurde des Maloti-Drakensberg Transfrontier Conservation Area (etwa: Maloti-Drakensberge-Grenzüberschreitendes-Erhaltungsgebiet) gegründet. Dieses verbindet den ukhahlamba-Drakensberg Park mit dem Sehlabathebe-Nationalpark in Lesotho. Ihm liegt der Anspruch an einen Peace Park (Transfrontier Conservation Area/TFCA) zugrunde. Die zwölf Kilometer lange Staatsgrenze kann zu Fuß passiert werden. Seit 2013 sind beide Nationalparks zusammen als Maloti Drakensberg Transboundary World Heritage Site in der UNESCO-Welterbe-Liste verzeichnet. Der gesamte Park ist nunmehr 2493 km² groß, wobei 65 km² der Fläche auf das Terrain Lesothos entfallen.
„… exceptional natural beauty in its soaring basaltic buttresses, incisive dramatic cutbacks, and golden sandstone ramparts … the site’s diversity of habitats protects a high level of endemic and globally threatened species, especially birds and plants … [and it] also contains many caves and rock-shelters with the largest and most concentrated group of paintings in Africa south of the Sahara. – … außergewöhnliche Schönheit der Natur in seinen aufragenden Basaltpfeilern, prägnante dramatische Einschnitte, und goldene Sandstein-Wälle … Die Vielfalt der Lebensräume beschützt ein hohes Maß an endemischen und vom Aussterben bedrohten Arten, vor allem Vögel und Pflanzen … [und es] enthält viele Höhlen und Felsnischen mit der größten und dichtesten Gruppe von Gemälden in Afrika südlich der Sahara.“
– Beschreibung des Maloti-Drakensberg Transfrontier Conservation Area auf der Website der UNESCO: Begründung zur Auswahl 2013
Teile der Drakensberg-Gebirgskette sind zu Schutzzwecken mit übergeordneter Bedeutung als Totalreservate ausgewiesen, sowie für touristische Zwecke daneben als Wildreservate. Entsprechend der Ramsar-Konvention wird der uKhahlamba Drakensberg Park auch als Schutzgut der List of Ramsar wetlands of international importance geführt. Private Eigentumsrechte hält an kleineren Gebietsteilen die Cathkin Estates Conservation and Wildlife Sanctuary.
(Wikipedia)
Der Royal Natal National Park wurde 1916 in den südafrikanischen Drakensbergen in der heutigen Provinz KwaZulu-Natal gebildet. Er ist Teil des Ukhahlamba-Drakensberg Park, der zum UNESCO-Welterbe gehört. Er gehört zu den spektakulärsten Natursehenswürdigkeiten in Afrika. Beeindruckend ist das Amphitheatre, eine mehrere Kilometer lange und etwa 1000 Meter hohe Felswand zwischen Sentinel (3165 m) und Eastern Buttress (3047 m). Auf dem flachen Gipfelplateau stehen einige Berge wie der Mont-Aux-Sources (Sesotho: Phofung) (3282 m), den 1836 die französischen Missionare Thomas Arbousset und François Daumas bestiegen und nach den Quellen von drei größeren Flüssen benannten.
Einer von diesen, der Tugela, stürzt in den Tugelafällen in fünf Stufen 948 Meter in die Tiefe (andere Angaben: knapp 3000 Fuß, 540 m). In kalten Wintern friert er in den oberen Stufen und bildet eindrucksvolle Eissäulen.
Der Royal Natal National Park ist ideal geeignet für Wanderungen mit einem Netz von klassifizierten Wegen aller Schwierigkeitsgrade; dies reicht von der leichten Besteigung des Mont-aux-Sources vom Plateau aus bis zur jährlichen Mont-aux-Sources Challenge, wenn Querfeldeinläufer zusammenkommen, um die 50 Kilometer lange Strecke in weniger als fünf Stunden zu absolvieren.
(Wikipedia)
Cathedral Peak - Hike around One Tree Hill
Cathedral Peak - Wanderung um den One Tree Hill
The uKhahlamba-Drakensberg Park is in the KwaZulu-Natal province of South Africa, covering 2,428.13 km2 (938 sq mi) of area. The park includes Royal Natal National Park, a provincial park, and covers part of the Drakensberg, the highest mountain range in Southern Africa.
The park and the adjoining Sehlabathebe National Park in the Kingdom of Lesotho are part of the Maloti-Drakensberg Park, which was first declared a World Heritage Site on 30 November 2000. It is described by UNESCO as having "exceptional natural beauty in its soaring basaltic buttresses, incisive dramatic cutbacks, and golden sandstone ramparts... the site’s diversity of habitats protects a high level of endemic and globally threatened species, especially birds and plants... [and it] also contains many caves and rock-shelters with the largest and most concentrated group of paintings in Africa south of the Sahara".
Plans to boost tourism in the area include a long-awaited cable car project by the KZN Economic Development, Tourism and Environmental Affairs Department.
The Drakensberg mountain range is characterized by a high level of endemism of both invertebrates and vertebrates.
Most of the higher South African parts of the Drakensberg mountain range have been designated as game reserves or wilderness areas. The uKhahlamba-Drakensberg Park is also in the List of Wetlands of International Importance (under the Ramsar Convention). Adjacent to the park is the Cathkin Estates Conservation and Wildlife Sanctuary, which spans 1,044 ha (10 km2) of virgin grassland and represents the largest privately owned game park in the KwaZulu-Natal Drakensberg region.
(Wikipedia)
Der uKhahlamba-Drakensberg Park (isiZulu uKhahlamba = „Barriere aus Speeren“) ist ein Nationalpark in den Drakensbergen in Südafrika. Im November 2000 wurde der Park in die UNESCO-Welterbe-Liste eingetragen. Der Park wird von der Provinzbehörde Ezemvelo KZN Wildlife verwaltet.
Der Park bedeckt eine Fläche von 2428 km². Er liegt in der Provinz KwaZulu-Natal und bildet einen 180 Kilometer langen und bis zu 20 Kilometer breiten Streifen entlang der Grenze zum Königreich Lesotho. Weitere Bestandteile des uKhahlamba-Drakensberg Park sind die getrennt liegenden Gebiete Royal-Natal-Nationalpark und Spioenkop Dam Nature Reserve weiter im Norden.
Der Park verfügt über hochaufragende Bergformationen und ist mit einem gut ausgebauten Netz von Wanderpfaden durchzogen. Basaltene, senkrecht aufragende Bergpfeiler, Bastionen aus goldbraunem Sandstein sowie skulpturierte Bögen, Höhlen, Säulen und Felswannen prägen das Landschaftsbild. Die Kette der Drakensberge im uKhahlamba-Drakensberg Park umfasst mehrere über 3000 Meter hohe Gipfel wie den Mafadi, den Giant’s Castle, den Cathedral Peak, den Monk’s Cowl, den Champagne Castle und den Njesuthi. Die Berghänge sind teilweise als Naturschutzgebiete ausgewiesen, in denen sich rund 30.000 Felsmalereien in etwa 600 Höhlen finden, die von San-Menschen über einen Zeitraum von 4000 Jahren erstellt wurden. In dieser Region entspringen die meisten großen Flüsse der Provinz KwaZulu-Natal. Sie bilden tiefe Schluchten und Täler. Einzige Straßenverbindung durch den Park nach Lesotho ist die Strecke über den Sanipass.
Es gibt eine Vielfalt endemischer Pflanzenarten, darunter Zuckerbüsche. Im Frühjahr übersäen in den Niederungen Teppiche von Wildblumen den Park, darunter Watsonia-Arten.
Zu den Vogelarten gehören Kapgeier (Gyps coprotheres) und Bartgeier (Gypaetus barbatus). Zahlreiche im Park beheimatete Wirbeltiere und Wirbellose sind endemisch. Weiterhin leben im Park Buschböcke, Ducker, Elenantilopen und Paviane.
1903 beschloss die Regierung der Kolonie Natal die Errichtung eines Naturschutzgebietes in den Drakensbergen. 1905 wurde eine klare Grenzziehung des Schutzbereichs proklamiert. 1916 wurde der Royal Natal National Park eingerichtet. Ab den 1950er Jahren wurden in den Drakensbergen diverse Naturschutzgebiete ausgewiesen, so 1951 das Kamberg Nature Reserve, 1953 das Nature Reserve de Lotheni und 1967 Vergelegen. Dabei wurde der Gewässerschutz vorangetrieben. 1973 kamen die Schutzgebiete Mdedelelo und Mkomazi hinzu.
Im Juni 2001 wurde des Maloti-Drakensberg Transfrontier Conservation Area (etwa: Maloti-Drakensberge-Grenzüberschreitendes-Erhaltungsgebiet) gegründet. Dieses verbindet den ukhahlamba-Drakensberg Park mit dem Sehlabathebe-Nationalpark in Lesotho. Ihm liegt der Anspruch an einen Peace Park (Transfrontier Conservation Area/TFCA) zugrunde. Die zwölf Kilometer lange Staatsgrenze kann zu Fuß passiert werden. Seit 2013 sind beide Nationalparks zusammen als Maloti Drakensberg Transboundary World Heritage Site in der UNESCO-Welterbe-Liste verzeichnet. Der gesamte Park ist nunmehr 2493 km² groß, wobei 65 km² der Fläche auf das Terrain Lesothos entfallen.
„… exceptional natural beauty in its soaring basaltic buttresses, incisive dramatic cutbacks, and golden sandstone ramparts … the site’s diversity of habitats protects a high level of endemic and globally threatened species, especially birds and plants … [and it] also contains many caves and rock-shelters with the largest and most concentrated group of paintings in Africa south of the Sahara. – … außergewöhnliche Schönheit der Natur in seinen aufragenden Basaltpfeilern, prägnante dramatische Einschnitte, und goldene Sandstein-Wälle … Die Vielfalt der Lebensräume beschützt ein hohes Maß an endemischen und vom Aussterben bedrohten Arten, vor allem Vögel und Pflanzen … [und es] enthält viele Höhlen und Felsnischen mit der größten und dichtesten Gruppe von Gemälden in Afrika südlich der Sahara.“
– Beschreibung des Maloti-Drakensberg Transfrontier Conservation Area auf der Website der UNESCO: Begründung zur Auswahl 2013
Teile der Drakensberg-Gebirgskette sind zu Schutzzwecken mit übergeordneter Bedeutung als Totalreservate ausgewiesen, sowie für touristische Zwecke daneben als Wildreservate. Entsprechend der Ramsar-Konvention wird der uKhahlamba Drakensberg Park auch als Schutzgut der List of Ramsar wetlands of international importance geführt. Private Eigentumsrechte hält an kleineren Gebietsteilen die Cathkin Estates Conservation and Wildlife Sanctuary.
(Wikipedia)
Lowveld View
The Blyde River Canyon, officially the Motlatse Canyon is a significant natural feature of South Africa, located in Mpumalanga, and forming the northern part of the Drakensberg escarpment. Located in the Blyde River Canyon Nature Reserve, it is 25 kilometres (16 mi) in length and is, on average, around 750 metres (2,461 ft) deep. The Blyderivierpoort Dam, when full, is at an altitude of 665 metres (2,182 ft). The canyon consists mostly of red sandstone. The highest point of the canyon, Mariepskop, is 1,944 metres (6,378 ft) above sea level, whilst its lowest point where the river leaves the canyon is slightly less than 561 metres (1,841 ft) above sea level. This means that by some measure the canyon is 1,383 metres (4,537 ft) deep.
While it is difficult to compare canyons world-wide, Blyde River Canyon is one of the largest canyons on Earth, and it may be the largest 'green canyon' due to its lush subtropical foliage. It has some of the deepest precipitous cliffs of any canyon on the planet. It is the second largest canyon in Africa, after the Fish River Canyon, and is known as one of the great wonders of nature on the continent.
Possibly the best view in the whole of the Blyde River Canyon is of the "Three Rondavels", huge, round rocks, thought to be reminiscent of the houses or huts of the indigenous people, known as rondavels. This canyon is part of the Panorama Route. This route starts at the town Graskop and includes God's Window, the Pinnacle and Bourke's Luck Potholes.
Blyde means "glad" or "happy" in old Dutch, a name derived from a voortrekkers' expedition. The 'happy river' was thus named in 1844, when Hendrik Potgieter and others returned safely from Delagoa Bay to the rest of their party of trekkers who had considered them dead. While still under this misapprehension they had named the nearby river where they had been encamped, Treurrivier, or 'mourning river'.
In 2005, the Blyde River was renamed to the Motlatse River, and the Mpumalanga Provincial Government announced that the canyon would be renamed as well.
The Blyde River Canyon supports large diversity of life, including numerous fish and antelope species as well as hippos and crocodiles, and every primate species that may be seen in South Africa (including both greater and lesser bushbabies, vervet monkeys and Samango monkeys). The diversity of birdlife is similarly high, including the beautiful and much sought Narina trogon as well as species such as the Cape vulture, black eagle, crowned eagle, African fish eagle, gymnogene, jackal buzzard, white-rumped vulture, bald ibis, African finfoot, Knysna lourie, purple-crested lourie, Gurney's sugarbird, malachite sunbird, cinnamon dove, African emerald cuckoo, red-backed mannikin, golden-tailed woodpecker, olive bush shrike, green twinspot, Taita falcons (very rarely sighted, a breeding pair lives in the nearby Abel Erasmus Pass), Cape eagle owl, white-faced owl, wood owl, peregrine falcon, black-breasted snake eagle, Wahlberg's eagle, long-crested eagle, lanner falcon, red-breasted sparrowhawk, rock kestrel and others.
At 200 metres (660 ft), the Kadishi Tufa waterfall is the second tallest tufa waterfall on earth. A tufa waterfall is formed when water running over dolomite rock absorbs calcium, and deposits rock formations more rapidly than they erode the surrounding rock. In the case of the Kadishi Tufa fall, the formation that has been produced strikingly resembles a face which is crying profusely, and is thus sometimes known as 'the weeping face of nature'.
The canyon and the surrounding Drakensberg escarpment is a very popular tourist region with a well-developed tourism industry supported by good public infrastructure.
(Wikipedia)
Der Blyde River Canyon ist ein 26 Kilometer langer, bis 800 Meter tiefer und hauptsächlich aus rotem Sandstein bestehender Canyon. Er befindet sich an der Panorama Route nordöstlich von Johannesburg und gilt als eines der großen Naturwunder Afrikas.
Durch den Blyde River Canyon, der an den Bourke’s Luck Potholes beginnt, fließt der Fluss Blyde River, der bei 25° 4′ 15,9″ S, 30° 40′ 40,2″ O dem Thaba Chweu entspringt und bei 24° 15′ 18,6″ S, 30° 49′ 50″ O in den Olifantsriver fließt.
Ein von zahlreichen Touristen besuchter Punkt des Canyons sind die drei Rondavels, gewaltige, runde Felsen, die an die runden Hütten der Einheimischen erinnern. Wegen seines Ausblicks vielbesucht ist auch God’s Window.
(Wikipedia)
Sunrise seen from Highlands Mountain Retreat.
Sonnenaufgang vom Highlands Mountain Retreat gesehen.
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 paleontology finds have been made in the park, including dinosaur eggs and skeletons.
"Golden Gate" refers to the sandstone cliffs found on either side of the valley at the Golden Gate dam. In 1875, a farmer called J.N.R. van Reenen and his wife stopped here as they travelled to their new farm in Vuurland. He named the location "Golden Gate" when he saw the last rays of the setting sun fall on the cliffs.
In 1963, 47.92 km2 (11,840 acres) were proclaimed as a national park, specifically to preserve the scenic beauty of the area. In 1981, the park was enlarged to 62.41 km2 (15,420 acres), and in 1988, it was enlarged to 116.33 km2 (28,750 acres). In 2004, the park was announced to be joining with the neighbouring QwaQwa National Park. The amalgamation of QwaQwa National Park was completed in 2007, increasing the park's area to 340 km2 (84,000 acres).
The park is 320 km (200 mi) from Johannesburg and is close to the villages of Clarens and Kestell, in the upper regions of the Little Caledon River. The park is situated in the Rooiberge of the eastern Free State, in the foothills of the Maluti Mountains. The Caledon River forms the southern boundary of the park, as well as the border between the Free State and Lesotho. The highest peak in the park (and also in the Free State) is Ribbokkop at 2,829 m (9,281 ft) above sea level.
The park is located in the eastern highveld region of South Africa, and experiences a dry, sunny climate from June to August. It has showers, hail, and thunderstorms between October and April. It has thick snowfalls in the winter. The park has a relatively high rainfall of 800 mm (31 in) per year.
The park is an area of rich highveld and montane grassland flora. It has more than 60 grass species and a large variety of bulbs and herbs. Each of these species has its own flowering time, meaning that veld flowers can be seen throughout the summer. The park also has Afromontane forests and high-altitude Austro-Afro alpine grassland, which is scarce in South Africa. The ouhout (Leucosidea sericea), an evergreen species, is the most common tree in the park. Ouhout is a favourite habitat of beetles and 117 species occur on these trees in the park. The Lombardi poplars and weeping willows in the park are introduced species, but are kept because of their cultural and historic connection with the eastern Free State. Other exotic species in the park, for example wattle and bluegum, are systematically eradicated.
Instead of reintroducing one of the "big five" into the park, the sungazer lizard and water mongoose were reintroduced. Twelve species of mice, 10 species of carnivores, and 10 antelope species have been recorded in the park. The grey rhebuck and the mountain reedbuck were present when the park was established.
The geology of the park provides very visual "textbook" examples of Southern Africa's geological history. The sandstone formations in the park form the upper part of the Karoo Supergroup. These formations were deposited during a period of aeolian deposition towards the end of the Triassic Period. At the time of deposition, the climate of the area the park covers was becoming progressively drier until arid desert conditions set in, resulting in a land of dunes and sandy desert, with occasional scattered oases. The deposition of the sandstones ended when lava flowed out over the desert 190 million years ago.
The following sequence of geological formations is visible in the park (starting from the bottom): the Molteno Formation, Elliott Formation, Clarens Formation, and Drakensberg Formation. The yellow-brown Golden Gate and Brandwag cliffs are made up of the Clarens formation. The layers in this formation are 140 to 160 m (460 to 520 ft) thick. The Drakensberg formation comprises the basaltic lava that flowed over the desert. It forms the mountain summits in the park. On Ribbokkop, it is 600 m (2,000 ft) thick. The Elliot Formation is a red mudstone where many dinosaur fossils have been found.
The oldest dinosaur embryos ever discovered were found in the park in 1978. The eggs were from the Triassic Period (220 to 195 million years ago) and had fossilised foetal skeletons of Massospondylus, a prosauropod dinosaur. More examples of these eggs have since been found in the park. Other fossils found in the park include those of advanced cynodontia (canine toothed animals), small thecodontia (animals with teeth set firmly in the jaw), and bird-like and crocodile-like dinosaurs.
Accommodation in the park is available at Glen Reenen and Brandwag Rest camps. Caravan and camp sites with all amenities are available at Glen Reenen camp. The hotel was formerly part of Brandwag camp, but since its recent refurbishment, it is managed separately by SANParks as Golden Gate Hotel. The nearest town to Golden Gate Highlands National Park is Clarens (17 km to the west), but Phuthaditjhaba is also easily reached by a good tar road, driving through the access gate to the east of the park.
This park will be included into the Maloti-Drakensberg Transfrontier Conservation Area, Peace Park.
(Wikipedia)
Der Golden-Gate-Highlands-Nationalpark (englisch Golden Gate Highlands National Park) liegt in Südafrika, im Südosten des Freistaates nahe der Grenze zu Lesotho, und zeichnet sich besonders durch seine malerischen Felslandschaften aus. Orange oder ocker gefärbte Sandsteinfelsen ragen über das bergige Grasland auf. Außerdem gibt es Felsmalereien der San.
Der nördliche Eingang zum Park liegt bei dem Künstlerdorf Clarens.
(Wikipedia)
Hike around Plowman's Kop via the Crack and Mudslide
Wanderung über den Plowman's Kop über Crack und Mudslide
The uKhahlamba-Drakensberg Park is in the KwaZulu-Natal province of South Africa, covering 2,428.13 km2 (938 sq mi) of area. The park includes Royal Natal National Park, a provincial park, and covers part of the Drakensberg, the highest mountain range in Southern Africa.
The park and the adjoining Sehlabathebe National Park in the Kingdom of Lesotho are part of the Maloti-Drakensberg Park, which was first declared a World Heritage Site on 30 November 2000. It is described by UNESCO as having "exceptional natural beauty in its soaring basaltic buttresses, incisive dramatic cutbacks, and golden sandstone ramparts... the site’s diversity of habitats protects a high level of endemic and globally threatened species, especially birds and plants... [and it] also contains many caves and rock-shelters with the largest and most concentrated group of paintings in Africa south of the Sahara".
Plans to boost tourism in the area include a long-awaited cable car project by the KZN Economic Development, Tourism and Environmental Affairs Department.
The Drakensberg mountain range is characterized by a high level of endemism of both invertebrates and vertebrates.
Most of the higher South African parts of the Drakensberg mountain range have been designated as game reserves or wilderness areas. The uKhahlamba-Drakensberg Park is also in the List of Wetlands of International Importance (under the Ramsar Convention). Adjacent to the park is the Cathkin Estates Conservation and Wildlife Sanctuary, which spans 1,044 ha (10 km2) of virgin grassland and represents the largest privately owned game park in the KwaZulu-Natal Drakensberg region.
(Wikipedia)
The Royal Natal National Park is in the KwaZulu Natal province of South Africa and forms part of the uKhahlamba Drakensberg Park World Heritage Site. Notwithstanding the name, it is actually not a South African National Park managed by the SANParks, but rather a Provincial Park managed by Ezemvelo KZN Wildlife. This park is now included into the Maloti-Drakensberg Transfrontier Conservation Area Peace Park.
The main features of the park are the Drakensberg Amphitheatre, a rock wall 5 kilometres (3.1 mi) long by up to 1,200 metres (3,900 ft) high, Mont-Aux-Sources peak where the Orange and Tugela rivers have their source, and the 948-metre (3,110 ft) Tugela Falls, the world's second-highest waterfall.
(Wikipedia)
Der uKhahlamba-Drakensberg Park (isiZulu uKhahlamba = „Barriere aus Speeren“) ist ein Nationalpark in den Drakensbergen in Südafrika. Im November 2000 wurde der Park in die UNESCO-Welterbe-Liste eingetragen. Der Park wird von der Provinzbehörde Ezemvelo KZN Wildlife verwaltet.
Der Park bedeckt eine Fläche von 2428 km². Er liegt in der Provinz KwaZulu-Natal und bildet einen 180 Kilometer langen und bis zu 20 Kilometer breiten Streifen entlang der Grenze zum Königreich Lesotho. Weitere Bestandteile des uKhahlamba-Drakensberg Park sind die getrennt liegenden Gebiete Royal-Natal-Nationalpark und Spioenkop Dam Nature Reserve weiter im Norden.
Der Park verfügt über hochaufragende Bergformationen und ist mit einem gut ausgebauten Netz von Wanderpfaden durchzogen. Basaltene, senkrecht aufragende Bergpfeiler, Bastionen aus goldbraunem Sandstein sowie skulpturierte Bögen, Höhlen, Säulen und Felswannen prägen das Landschaftsbild. Die Kette der Drakensberge im uKhahlamba-Drakensberg Park umfasst mehrere über 3000 Meter hohe Gipfel wie den Mafadi, den Giant’s Castle, den Cathedral Peak, den Monk’s Cowl, den Champagne Castle und den Njesuthi. Die Berghänge sind teilweise als Naturschutzgebiete ausgewiesen, in denen sich rund 30.000 Felsmalereien in etwa 600 Höhlen finden, die von San-Menschen über einen Zeitraum von 4000 Jahren erstellt wurden. In dieser Region entspringen die meisten großen Flüsse der Provinz KwaZulu-Natal. Sie bilden tiefe Schluchten und Täler. Einzige Straßenverbindung durch den Park nach Lesotho ist die Strecke über den Sanipass.
Es gibt eine Vielfalt endemischer Pflanzenarten, darunter Zuckerbüsche. Im Frühjahr übersäen in den Niederungen Teppiche von Wildblumen den Park, darunter Watsonia-Arten.
Zu den Vogelarten gehören Kapgeier (Gyps coprotheres) und Bartgeier (Gypaetus barbatus). Zahlreiche im Park beheimatete Wirbeltiere und Wirbellose sind endemisch. Weiterhin leben im Park Buschböcke, Ducker, Elenantilopen und Paviane.
1903 beschloss die Regierung der Kolonie Natal die Errichtung eines Naturschutzgebietes in den Drakensbergen. 1905 wurde eine klare Grenzziehung des Schutzbereichs proklamiert. 1916 wurde der Royal Natal National Park eingerichtet. Ab den 1950er Jahren wurden in den Drakensbergen diverse Naturschutzgebiete ausgewiesen, so 1951 das Kamberg Nature Reserve, 1953 das Nature Reserve de Lotheni und 1967 Vergelegen. Dabei wurde der Gewässerschutz vorangetrieben. 1973 kamen die Schutzgebiete Mdedelelo und Mkomazi hinzu.
Im Juni 2001 wurde des Maloti-Drakensberg Transfrontier Conservation Area (etwa: Maloti-Drakensberge-Grenzüberschreitendes-Erhaltungsgebiet) gegründet. Dieses verbindet den ukhahlamba-Drakensberg Park mit dem Sehlabathebe-Nationalpark in Lesotho. Ihm liegt der Anspruch an einen Peace Park (Transfrontier Conservation Area/TFCA) zugrunde. Die zwölf Kilometer lange Staatsgrenze kann zu Fuß passiert werden. Seit 2013 sind beide Nationalparks zusammen als Maloti Drakensberg Transboundary World Heritage Site in der UNESCO-Welterbe-Liste verzeichnet. Der gesamte Park ist nunmehr 2493 km² groß, wobei 65 km² der Fläche auf das Terrain Lesothos entfallen.
„… exceptional natural beauty in its soaring basaltic buttresses, incisive dramatic cutbacks, and golden sandstone ramparts … the site’s diversity of habitats protects a high level of endemic and globally threatened species, especially birds and plants … [and it] also contains many caves and rock-shelters with the largest and most concentrated group of paintings in Africa south of the Sahara. – … außergewöhnliche Schönheit der Natur in seinen aufragenden Basaltpfeilern, prägnante dramatische Einschnitte, und goldene Sandstein-Wälle … Die Vielfalt der Lebensräume beschützt ein hohes Maß an endemischen und vom Aussterben bedrohten Arten, vor allem Vögel und Pflanzen … [und es] enthält viele Höhlen und Felsnischen mit der größten und dichtesten Gruppe von Gemälden in Afrika südlich der Sahara.“
– Beschreibung des Maloti-Drakensberg Transfrontier Conservation Area auf der Website der UNESCO: Begründung zur Auswahl 2013
Teile der Drakensberg-Gebirgskette sind zu Schutzzwecken mit übergeordneter Bedeutung als Totalreservate ausgewiesen, sowie für touristische Zwecke daneben als Wildreservate. Entsprechend der Ramsar-Konvention wird der uKhahlamba Drakensberg Park auch als Schutzgut der List of Ramsar wetlands of international importance geführt. Private Eigentumsrechte hält an kleineren Gebietsteilen die Cathkin Estates Conservation and Wildlife Sanctuary.
(Wikipedia)
Der Royal Natal National Park wurde 1916 in den südafrikanischen Drakensbergen in der heutigen Provinz KwaZulu-Natal gebildet. Er ist Teil des Ukhahlamba-Drakensberg Park, der zum UNESCO-Welterbe gehört. Er gehört zu den spektakulärsten Natursehenswürdigkeiten in Afrika. Beeindruckend ist das Amphitheatre, eine mehrere Kilometer lange und etwa 1000 Meter hohe Felswand zwischen Sentinel (3165 m) und Eastern Buttress (3047 m). Auf dem flachen Gipfelplateau stehen einige Berge wie der Mont-Aux-Sources (Sesotho: Phofung) (3282 m), den 1836 die französischen Missionare Thomas Arbousset und François Daumas bestiegen und nach den Quellen von drei größeren Flüssen benannten.
Einer von diesen, der Tugela, stürzt in den Tugelafällen in fünf Stufen 948 Meter in die Tiefe (andere Angaben: knapp 3000 Fuß, 540 m). In kalten Wintern friert er in den oberen Stufen und bildet eindrucksvolle Eissäulen.
Der Royal Natal National Park ist ideal geeignet für Wanderungen mit einem Netz von klassifizierten Wegen aller Schwierigkeitsgrade; dies reicht von der leichten Besteigung des Mont-aux-Sources vom Plateau aus bis zur jährlichen Mont-aux-Sources Challenge, wenn Querfeldeinläufer zusammenkommen, um die 50 Kilometer lange Strecke in weniger als fünf Stunden zu absolvieren.
(Wikipedia)
Sunrise
Amphitheatre seen from Upper Thendele Camp. In the foreground you can see the Policeman's Helmet.
Sonnenaufgang
Amphitheater
vom Upper Thendele Camp aus gesehen. Im Vordergrund sieht man den Policeman's Helmet.
The uKhahlamba-Drakensberg Park is in the KwaZulu-Natal province of South Africa, covering 2,428.13 km2 (938 sq mi) of area. The park includes Royal Natal National Park, a provincial park, and covers part of the Drakensberg, the highest mountain range in Southern Africa.
The park and the adjoining Sehlabathebe National Park in the Kingdom of Lesotho are part of the Maloti-Drakensberg Park, which was first declared a World Heritage Site on 30 November 2000. It is described by UNESCO as having "exceptional natural beauty in its soaring basaltic buttresses, incisive dramatic cutbacks, and golden sandstone ramparts... the site’s diversity of habitats protects a high level of endemic and globally threatened species, especially birds and plants... [and it] also contains many caves and rock-shelters with the largest and most concentrated group of paintings in Africa south of the Sahara".
Plans to boost tourism in the area include a long-awaited cable car project by the KZN Economic Development, Tourism and Environmental Affairs Department.
The Drakensberg mountain range is characterized by a high level of endemism of both invertebrates and vertebrates.
Most of the higher South African parts of the Drakensberg mountain range have been designated as game reserves or wilderness areas. The uKhahlamba-Drakensberg Park is also in the List of Wetlands of International Importance (under the Ramsar Convention). Adjacent to the park is the Cathkin Estates Conservation and Wildlife Sanctuary, which spans 1,044 ha (10 km2) of virgin grassland and represents the largest privately owned game park in the KwaZulu-Natal Drakensberg region.
(Wikipedia)
The Royal Natal National Park is in the KwaZulu Natal province of South Africa and forms part of the uKhahlamba Drakensberg Park World Heritage Site. Notwithstanding the name, it is actually not a South African National Park managed by the SANParks, but rather a Provincial Park managed by Ezemvelo KZN Wildlife. This park is now included into the Maloti-Drakensberg Transfrontier Conservation Area Peace Park.
The main features of the park are the Drakensberg Amphitheatre, a rock wall 5 kilometres (3.1 mi) long by up to 1,200 metres (3,900 ft) high, Mont-Aux-Sources peak where the Orange and Tugela rivers have their source, and the 948-metre (3,110 ft) Tugela Falls, the world's second-highest waterfall.
(Wikipedia)
Der uKhahlamba-Drakensberg Park (isiZulu uKhahlamba = „Barriere aus Speeren“) ist ein Nationalpark in den Drakensbergen in Südafrika. Im November 2000 wurde der Park in die UNESCO-Welterbe-Liste eingetragen. Der Park wird von der Provinzbehörde Ezemvelo KZN Wildlife verwaltet.
Der Park bedeckt eine Fläche von 2428 km². Er liegt in der Provinz KwaZulu-Natal und bildet einen 180 Kilometer langen und bis zu 20 Kilometer breiten Streifen entlang der Grenze zum Königreich Lesotho. Weitere Bestandteile des uKhahlamba-Drakensberg Park sind die getrennt liegenden Gebiete Royal-Natal-Nationalpark und Spioenkop Dam Nature Reserve weiter im Norden.
Der Park verfügt über hochaufragende Bergformationen und ist mit einem gut ausgebauten Netz von Wanderpfaden durchzogen. Basaltene, senkrecht aufragende Bergpfeiler, Bastionen aus goldbraunem Sandstein sowie skulpturierte Bögen, Höhlen, Säulen und Felswannen prägen das Landschaftsbild. Die Kette der Drakensberge im uKhahlamba-Drakensberg Park umfasst mehrere über 3000 Meter hohe Gipfel wie den Mafadi, den Giant’s Castle, den Cathedral Peak, den Monk’s Cowl, den Champagne Castle und den Njesuthi. Die Berghänge sind teilweise als Naturschutzgebiete ausgewiesen, in denen sich rund 30.000 Felsmalereien in etwa 600 Höhlen finden, die von San-Menschen über einen Zeitraum von 4000 Jahren erstellt wurden. In dieser Region entspringen die meisten großen Flüsse der Provinz KwaZulu-Natal. Sie bilden tiefe Schluchten und Täler. Einzige Straßenverbindung durch den Park nach Lesotho ist die Strecke über den Sanipass.
Es gibt eine Vielfalt endemischer Pflanzenarten, darunter Zuckerbüsche. Im Frühjahr übersäen in den Niederungen Teppiche von Wildblumen den Park, darunter Watsonia-Arten.
Zu den Vogelarten gehören Kapgeier (Gyps coprotheres) und Bartgeier (Gypaetus barbatus). Zahlreiche im Park beheimatete Wirbeltiere und Wirbellose sind endemisch. Weiterhin leben im Park Buschböcke, Ducker, Elenantilopen und Paviane.
1903 beschloss die Regierung der Kolonie Natal die Errichtung eines Naturschutzgebietes in den Drakensbergen. 1905 wurde eine klare Grenzziehung des Schutzbereichs proklamiert. 1916 wurde der Royal Natal National Park eingerichtet. Ab den 1950er Jahren wurden in den Drakensbergen diverse Naturschutzgebiete ausgewiesen, so 1951 das Kamberg Nature Reserve, 1953 das Nature Reserve de Lotheni und 1967 Vergelegen. Dabei wurde der Gewässerschutz vorangetrieben. 1973 kamen die Schutzgebiete Mdedelelo und Mkomazi hinzu.
Im Juni 2001 wurde des Maloti-Drakensberg Transfrontier Conservation Area (etwa: Maloti-Drakensberge-Grenzüberschreitendes-Erhaltungsgebiet) gegründet. Dieses verbindet den ukhahlamba-Drakensberg Park mit dem Sehlabathebe-Nationalpark in Lesotho. Ihm liegt der Anspruch an einen Peace Park (Transfrontier Conservation Area/TFCA) zugrunde. Die zwölf Kilometer lange Staatsgrenze kann zu Fuß passiert werden. Seit 2013 sind beide Nationalparks zusammen als Maloti Drakensberg Transboundary World Heritage Site in der UNESCO-Welterbe-Liste verzeichnet. Der gesamte Park ist nunmehr 2493 km² groß, wobei 65 km² der Fläche auf das Terrain Lesothos entfallen.
„… exceptional natural beauty in its soaring basaltic buttresses, incisive dramatic cutbacks, and golden sandstone ramparts … the site’s diversity of habitats protects a high level of endemic and globally threatened species, especially birds and plants … [and it] also contains many caves and rock-shelters with the largest and most concentrated group of paintings in Africa south of the Sahara. – … außergewöhnliche Schönheit der Natur in seinen aufragenden Basaltpfeilern, prägnante dramatische Einschnitte, und goldene Sandstein-Wälle … Die Vielfalt der Lebensräume beschützt ein hohes Maß an endemischen und vom Aussterben bedrohten Arten, vor allem Vögel und Pflanzen … [und es] enthält viele Höhlen und Felsnischen mit der größten und dichtesten Gruppe von Gemälden in Afrika südlich der Sahara.“
– Beschreibung des Maloti-Drakensberg Transfrontier Conservation Area auf der Website der UNESCO: Begründung zur Auswahl 2013
Teile der Drakensberg-Gebirgskette sind zu Schutzzwecken mit übergeordneter Bedeutung als Totalreservate ausgewiesen, sowie für touristische Zwecke daneben als Wildreservate. Entsprechend der Ramsar-Konvention wird der uKhahlamba Drakensberg Park auch als Schutzgut der List of Ramsar wetlands of international importance geführt. Private Eigentumsrechte hält an kleineren Gebietsteilen die Cathkin Estates Conservation and Wildlife Sanctuary.
(Wikipedia)
Der Royal Natal National Park wurde 1916 in den südafrikanischen Drakensbergen in der heutigen Provinz KwaZulu-Natal gebildet. Er ist Teil des Ukhahlamba-Drakensberg Park, der zum UNESCO-Welterbe gehört. Er gehört zu den spektakulärsten Natursehenswürdigkeiten in Afrika. Beeindruckend ist das Amphitheatre, eine mehrere Kilometer lange und etwa 1000 Meter hohe Felswand zwischen Sentinel (3165 m) und Eastern Buttress (3047 m). Auf dem flachen Gipfelplateau stehen einige Berge wie der Mont-Aux-Sources (Sesotho: Phofung) (3282 m), den 1836 die französischen Missionare Thomas Arbousset und François Daumas bestiegen und nach den Quellen von drei größeren Flüssen benannten.
Einer von diesen, der Tugela, stürzt in den Tugelafällen in fünf Stufen 948 Meter in die Tiefe (andere Angaben: knapp 3000 Fuß, 540 m). In kalten Wintern friert er in den oberen Stufen und bildet eindrucksvolle Eissäulen.
Der Royal Natal National Park ist ideal geeignet für Wanderungen mit einem Netz von klassifizierten Wegen aller Schwierigkeitsgrade; dies reicht von der leichten Besteigung des Mont-aux-Sources vom Plateau aus bis zur jährlichen Mont-aux-Sources Challenge, wenn Querfeldeinläufer zusammenkommen, um die 50 Kilometer lange Strecke in weniger als fünf Stunden zu absolvieren.
(Wikipedia)
Die Berliner Skyline - heute am 14. November mit dem Super-Vollmond vom Drachenberg aus! Ich hoffe euch gefällt das Bild :)
©Patrick Lemoine
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Three Rondavels - Sunset
Three Rondavels - Sonnenuntergang
The Blyde River Canyon, officially the Motlatse Canyon is a significant natural feature of South Africa, located in Mpumalanga, and forming the northern part of the Drakensberg escarpment. Located in the Blyde River Canyon Nature Reserve, it is 25 kilometres (16 mi) in length and is, on average, around 750 metres (2,461 ft) deep. The Blyderivierpoort Dam, when full, is at an altitude of 665 metres (2,182 ft). The canyon consists mostly of red sandstone. The highest point of the canyon, Mariepskop, is 1,944 metres (6,378 ft) above sea level, whilst its lowest point where the river leaves the canyon is slightly less than 561 metres (1,841 ft) above sea level. This means that by some measure the canyon is 1,383 metres (4,537 ft) deep.
While it is difficult to compare canyons world-wide, Blyde River Canyon is one of the largest canyons on Earth, and it may be the largest 'green canyon' due to its lush subtropical foliage. It has some of the deepest precipitous cliffs of any canyon on the planet. It is the second largest canyon in Africa, after the Fish River Canyon, and is known as one of the great wonders of nature on the continent.
Possibly the best view in the whole of the Blyde River Canyon is of the "Three Rondavels", huge, round rocks, thought to be reminiscent of the houses or huts of the indigenous people, known as rondavels. This canyon is part of the Panorama Route. This route starts at the town Graskop and includes God's Window, the Pinnacle and Bourke's Luck Potholes.
Blyde means "glad" or "happy" in old Dutch, a name derived from a voortrekkers' expedition. The 'happy river' was thus named in 1844, when Hendrik Potgieter and others returned safely from Delagoa Bay to the rest of their party of trekkers who had considered them dead. While still under this misapprehension they had named the nearby river where they had been encamped, Treurrivier, or 'mourning river'.
In 2005, the Blyde River was renamed to the Motlatse River, and the Mpumalanga Provincial Government announced that the canyon would be renamed as well.
The Blyde River Canyon supports large diversity of life, including numerous fish and antelope species as well as hippos and crocodiles, and every primate species that may be seen in South Africa (including both greater and lesser bushbabies, vervet monkeys and Samango monkeys). The diversity of birdlife is similarly high, including the beautiful and much sought Narina trogon as well as species such as the Cape vulture, black eagle, crowned eagle, African fish eagle, gymnogene, jackal buzzard, white-rumped vulture, bald ibis, African finfoot, Knysna lourie, purple-crested lourie, Gurney's sugarbird, malachite sunbird, cinnamon dove, African emerald cuckoo, red-backed mannikin, golden-tailed woodpecker, olive bush shrike, green twinspot, Taita falcons (very rarely sighted, a breeding pair lives in the nearby Abel Erasmus Pass), Cape eagle owl, white-faced owl, wood owl, peregrine falcon, black-breasted snake eagle, Wahlberg's eagle, long-crested eagle, lanner falcon, red-breasted sparrowhawk, rock kestrel and others.
At 200 metres (660 ft), the Kadishi Tufa waterfall is the second tallest tufa waterfall on earth. A tufa waterfall is formed when water running over dolomite rock absorbs calcium, and deposits rock formations more rapidly than they erode the surrounding rock. In the case of the Kadishi Tufa fall, the formation that has been produced strikingly resembles a face which is crying profusely, and is thus sometimes known as 'the weeping face of nature'.
The canyon and the surrounding Drakensberg escarpment is a very popular tourist region with a well-developed tourism industry supported by good public infrastructure.
(Wikipedia)
The Three Rondavels are three round, grass-covered mountain tops with somewhat pointed peaks. They resemble the traditional round or oval rondavels or African homesteads quite closely, which are made with local materials. Sometimes they are also called the Three Sisters, though this may confuse them with a similar threesome visible from the N1 road in the Northern Cape, very far to the south.
The names of the peaks commemorate a 19th century chief, Maripi, and three of his wives. The flat-topped peak adjacent to the rondavels is Mapjaneng, "the chief", who is remembered for opposing invading Swazis in a memorable battle. The three rondavels are named for three of his more troublesome wives – Magabolle, Mogoladikwe and Maseroto. Behind the rondavels the distant high plateau of Mariepskop may be visible. Beside the dam, the isolated Thabaneng hill is known as the "sundial" or “mountain with a shadow that moves". It is said that the position of its shadow indicates the time of day.
On a clear day the lookout point provides extensive views. From here one looks over the canyon to the Three Rondavels on the other side, which is flanked on various sides by promontories of the northern Drakensberg range.
The formation of the attractive sedimentary formations are explained geologically as the slow erosion of underlying soft stone, leaving the exposed the more resistant quartzite and shale rondavels.
(Wikipedia)
Der Blyde River Canyon ist ein 26 Kilometer langer, bis 800 Meter tiefer und hauptsächlich aus rotem Sandstein bestehender Canyon. Er befindet sich an der Panorama Route nordöstlich von Johannesburg und gilt als eines der großen Naturwunder Afrikas.
Durch den Blyde River Canyon, der an den Bourke’s Luck Potholes beginnt, fließt der Fluss Blyde River, der bei 25° 4′ 15,9″ S, 30° 40′ 40,2″ O dem Thaba Chweu entspringt und bei 24° 15′ 18,6″ S, 30° 49′ 50″ O in den Olifantsriver fließt.
Ein von zahlreichen Touristen besuchter Punkt des Canyons sind die drei Rondavels, gewaltige, runde Felsen, die an die runden Hütten der Einheimischen erinnern. Wegen seines Ausblicks vielbesucht ist auch God’s Window.
(Wikipedia)
Thukela Gorge Hike
Wanderung in die Thukela Schlucht
The uKhahlamba-Drakensberg Park is in the KwaZulu-Natal province of South Africa, covering 2,428.13 km2 (938 sq mi) of area. The park includes Royal Natal National Park, a provincial park, and covers part of the Drakensberg, the highest mountain range in Southern Africa.
The park and the adjoining Sehlabathebe National Park in the Kingdom of Lesotho are part of the Maloti-Drakensberg Park, which was first declared a World Heritage Site on 30 November 2000. It is described by UNESCO as having "exceptional natural beauty in its soaring basaltic buttresses, incisive dramatic cutbacks, and golden sandstone ramparts... the site’s diversity of habitats protects a high level of endemic and globally threatened species, especially birds and plants... [and it] also contains many caves and rock-shelters with the largest and most concentrated group of paintings in Africa south of the Sahara".
Plans to boost tourism in the area include a long-awaited cable car project by the KZN Economic Development, Tourism and Environmental Affairs Department.
The Drakensberg mountain range is characterized by a high level of endemism of both invertebrates and vertebrates.
Most of the higher South African parts of the Drakensberg mountain range have been designated as game reserves or wilderness areas. The uKhahlamba-Drakensberg Park is also in the List of Wetlands of International Importance (under the Ramsar Convention). Adjacent to the park is the Cathkin Estates Conservation and Wildlife Sanctuary, which spans 1,044 ha (10 km2) of virgin grassland and represents the largest privately owned game park in the KwaZulu-Natal Drakensberg region.
(Wikipedia)
The Royal Natal National Park is in the KwaZulu Natal province of South Africa and forms part of the uKhahlamba Drakensberg Park World Heritage Site. Notwithstanding the name, it is actually not a South African National Park managed by the SANParks, but rather a Provincial Park managed by Ezemvelo KZN Wildlife. This park is now included into the Maloti-Drakensberg Transfrontier Conservation Area Peace Park.
The main features of the park are the Drakensberg Amphitheatre, a rock wall 5 kilometres (3.1 mi) long by up to 1,200 metres (3,900 ft) high, Mont-Aux-Sources peak where the Orange and Tugela rivers have their source, and the 948-metre (3,110 ft) Tugela Falls, the world's second-highest waterfall.
(Wikipedia)
Der uKhahlamba-Drakensberg Park (isiZulu uKhahlamba = „Barriere aus Speeren“) ist ein Nationalpark in den Drakensbergen in Südafrika. Im November 2000 wurde der Park in die UNESCO-Welterbe-Liste eingetragen. Der Park wird von der Provinzbehörde Ezemvelo KZN Wildlife verwaltet.
Der Park bedeckt eine Fläche von 2428 km². Er liegt in der Provinz KwaZulu-Natal und bildet einen 180 Kilometer langen und bis zu 20 Kilometer breiten Streifen entlang der Grenze zum Königreich Lesotho. Weitere Bestandteile des uKhahlamba-Drakensberg Park sind die getrennt liegenden Gebiete Royal-Natal-Nationalpark und Spioenkop Dam Nature Reserve weiter im Norden.
Der Park verfügt über hochaufragende Bergformationen und ist mit einem gut ausgebauten Netz von Wanderpfaden durchzogen. Basaltene, senkrecht aufragende Bergpfeiler, Bastionen aus goldbraunem Sandstein sowie skulpturierte Bögen, Höhlen, Säulen und Felswannen prägen das Landschaftsbild. Die Kette der Drakensberge im uKhahlamba-Drakensberg Park umfasst mehrere über 3000 Meter hohe Gipfel wie den Mafadi, den Giant’s Castle, den Cathedral Peak, den Monk’s Cowl, den Champagne Castle und den Njesuthi. Die Berghänge sind teilweise als Naturschutzgebiete ausgewiesen, in denen sich rund 30.000 Felsmalereien in etwa 600 Höhlen finden, die von San-Menschen über einen Zeitraum von 4000 Jahren erstellt wurden. In dieser Region entspringen die meisten großen Flüsse der Provinz KwaZulu-Natal. Sie bilden tiefe Schluchten und Täler. Einzige Straßenverbindung durch den Park nach Lesotho ist die Strecke über den Sanipass.
Es gibt eine Vielfalt endemischer Pflanzenarten, darunter Zuckerbüsche. Im Frühjahr übersäen in den Niederungen Teppiche von Wildblumen den Park, darunter Watsonia-Arten.
Zu den Vogelarten gehören Kapgeier (Gyps coprotheres) und Bartgeier (Gypaetus barbatus). Zahlreiche im Park beheimatete Wirbeltiere und Wirbellose sind endemisch. Weiterhin leben im Park Buschböcke, Ducker, Elenantilopen und Paviane.
1903 beschloss die Regierung der Kolonie Natal die Errichtung eines Naturschutzgebietes in den Drakensbergen. 1905 wurde eine klare Grenzziehung des Schutzbereichs proklamiert. 1916 wurde der Royal Natal National Park eingerichtet. Ab den 1950er Jahren wurden in den Drakensbergen diverse Naturschutzgebiete ausgewiesen, so 1951 das Kamberg Nature Reserve, 1953 das Nature Reserve de Lotheni und 1967 Vergelegen. Dabei wurde der Gewässerschutz vorangetrieben. 1973 kamen die Schutzgebiete Mdedelelo und Mkomazi hinzu.
Im Juni 2001 wurde des Maloti-Drakensberg Transfrontier Conservation Area (etwa: Maloti-Drakensberge-Grenzüberschreitendes-Erhaltungsgebiet) gegründet. Dieses verbindet den ukhahlamba-Drakensberg Park mit dem Sehlabathebe-Nationalpark in Lesotho. Ihm liegt der Anspruch an einen Peace Park (Transfrontier Conservation Area/TFCA) zugrunde. Die zwölf Kilometer lange Staatsgrenze kann zu Fuß passiert werden. Seit 2013 sind beide Nationalparks zusammen als Maloti Drakensberg Transboundary World Heritage Site in der UNESCO-Welterbe-Liste verzeichnet. Der gesamte Park ist nunmehr 2493 km² groß, wobei 65 km² der Fläche auf das Terrain Lesothos entfallen.
„… exceptional natural beauty in its soaring basaltic buttresses, incisive dramatic cutbacks, and golden sandstone ramparts … the site’s diversity of habitats protects a high level of endemic and globally threatened species, especially birds and plants … [and it] also contains many caves and rock-shelters with the largest and most concentrated group of paintings in Africa south of the Sahara. – … außergewöhnliche Schönheit der Natur in seinen aufragenden Basaltpfeilern, prägnante dramatische Einschnitte, und goldene Sandstein-Wälle … Die Vielfalt der Lebensräume beschützt ein hohes Maß an endemischen und vom Aussterben bedrohten Arten, vor allem Vögel und Pflanzen … [und es] enthält viele Höhlen und Felsnischen mit der größten und dichtesten Gruppe von Gemälden in Afrika südlich der Sahara.“
– Beschreibung des Maloti-Drakensberg Transfrontier Conservation Area auf der Website der UNESCO: Begründung zur Auswahl 2013
Teile der Drakensberg-Gebirgskette sind zu Schutzzwecken mit übergeordneter Bedeutung als Totalreservate ausgewiesen, sowie für touristische Zwecke daneben als Wildreservate. Entsprechend der Ramsar-Konvention wird der uKhahlamba Drakensberg Park auch als Schutzgut der List of Ramsar wetlands of international importance geführt. Private Eigentumsrechte hält an kleineren Gebietsteilen die Cathkin Estates Conservation and Wildlife Sanctuary.
(Wikipedia)
Der Royal Natal National Park wurde 1916 in den südafrikanischen Drakensbergen in der heutigen Provinz KwaZulu-Natal gebildet. Er ist Teil des Ukhahlamba-Drakensberg Park, der zum UNESCO-Welterbe gehört. Er gehört zu den spektakulärsten Natursehenswürdigkeiten in Afrika. Beeindruckend ist das Amphitheatre, eine mehrere Kilometer lange und etwa 1000 Meter hohe Felswand zwischen Sentinel (3165 m) und Eastern Buttress (3047 m). Auf dem flachen Gipfelplateau stehen einige Berge wie der Mont-Aux-Sources (Sesotho: Phofung) (3282 m), den 1836 die französischen Missionare Thomas Arbousset und François Daumas bestiegen und nach den Quellen von drei größeren Flüssen benannten.
Einer von diesen, der Tugela, stürzt in den Tugelafällen in fünf Stufen 948 Meter in die Tiefe (andere Angaben: knapp 3000 Fuß, 540 m). In kalten Wintern friert er in den oberen Stufen und bildet eindrucksvolle Eissäulen.
Der Royal Natal National Park ist ideal geeignet für Wanderungen mit einem Netz von klassifizierten Wegen aller Schwierigkeitsgrade; dies reicht von der leichten Besteigung des Mont-aux-Sources vom Plateau aus bis zur jährlichen Mont-aux-Sources Challenge, wenn Querfeldeinläufer zusammenkommen, um die 50 Kilometer lange Strecke in weniger als fünf Stunden zu absolvieren.
(Wikipedia)
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 paleontology finds have been made in the park, including dinosaur eggs and skeletons.
"Golden Gate" refers to the sandstone cliffs found on either side of the valley at the Golden Gate dam. In 1875, a farmer called J.N.R. van Reenen and his wife stopped here as they travelled to their new farm in Vuurland. He named the location "Golden Gate" when he saw the last rays of the setting sun fall on the cliffs.
In 1963, 47.92 km2 (11,840 acres) were proclaimed as a national park, specifically to preserve the scenic beauty of the area. In 1981, the park was enlarged to 62.41 km2 (15,420 acres), and in 1988, it was enlarged to 116.33 km2 (28,750 acres). In 2004, the park was announced to be joining with the neighbouring QwaQwa National Park. The amalgamation of QwaQwa National Park was completed in 2007, increasing the park's area to 340 km2 (84,000 acres).
The park is 320 km (200 mi) from Johannesburg and is close to the villages of Clarens and Kestell, in the upper regions of the Little Caledon River. The park is situated in the Rooiberge of the eastern Free State, in the foothills of the Maluti Mountains. The Caledon River forms the southern boundary of the park, as well as the border between the Free State and Lesotho. The highest peak in the park (and also in the Free State) is Ribbokkop at 2,829 m (9,281 ft) above sea level.
The park is located in the eastern highveld region of South Africa, and experiences a dry, sunny climate from June to August. It has showers, hail, and thunderstorms between October and April. It has thick snowfalls in the winter. The park has a relatively high rainfall of 800 mm (31 in) per year.
The park is an area of rich highveld and montane grassland flora. It has more than 60 grass species and a large variety of bulbs and herbs. Each of these species has its own flowering time, meaning that veld flowers can be seen throughout the summer. The park also has Afromontane forests and high-altitude Austro-Afro alpine grassland, which is scarce in South Africa. The ouhout (Leucosidea sericea), an evergreen species, is the most common tree in the park. Ouhout is a favourite habitat of beetles and 117 species occur on these trees in the park. The Lombardi poplars and weeping willows in the park are introduced species, but are kept because of their cultural and historic connection with the eastern Free State. Other exotic species in the park, for example wattle and bluegum, are systematically eradicated.
Instead of reintroducing one of the "big five" into the park, the sungazer lizard and water mongoose were reintroduced. Twelve species of mice, 10 species of carnivores, and 10 antelope species have been recorded in the park. The grey rhebuck and the mountain reedbuck were present when the park was established.
The geology of the park provides very visual "textbook" examples of Southern Africa's geological history. The sandstone formations in the park form the upper part of the Karoo Supergroup. These formations were deposited during a period of aeolian deposition towards the end of the Triassic Period. At the time of deposition, the climate of the area the park covers was becoming progressively drier until arid desert conditions set in, resulting in a land of dunes and sandy desert, with occasional scattered oases. The deposition of the sandstones ended when lava flowed out over the desert 190 million years ago.
The following sequence of geological formations is visible in the park (starting from the bottom): the Molteno Formation, Elliott Formation, Clarens Formation, and Drakensberg Formation. The yellow-brown Golden Gate and Brandwag cliffs are made up of the Clarens formation. The layers in this formation are 140 to 160 m (460 to 520 ft) thick. The Drakensberg formation comprises the basaltic lava that flowed over the desert. It forms the mountain summits in the park. On Ribbokkop, it is 600 m (2,000 ft) thick. The Elliot Formation is a red mudstone where many dinosaur fossils have been found.
The oldest dinosaur embryos ever discovered were found in the park in 1978. The eggs were from the Triassic Period (220 to 195 million years ago) and had fossilised foetal skeletons of Massospondylus, a prosauropod dinosaur. More examples of these eggs have since been found in the park. Other fossils found in the park include those of advanced cynodontia (canine toothed animals), small thecodontia (animals with teeth set firmly in the jaw), and bird-like and crocodile-like dinosaurs.
Accommodation in the park is available at Glen Reenen and Brandwag Rest camps. Caravan and camp sites with all amenities are available at Glen Reenen camp. The hotel was formerly part of Brandwag camp, but since its recent refurbishment, it is managed separately by SANParks as Golden Gate Hotel. The nearest town to Golden Gate Highlands National Park is Clarens (17 km to the west), but Phuthaditjhaba is also easily reached by a good tar road, driving through the access gate to the east of the park.
This park will be included into the Maloti-Drakensberg Transfrontier Conservation Area, Peace Park.
(Wikipedia)
Der Golden-Gate-Highlands-Nationalpark (englisch Golden Gate Highlands National Park) liegt in Südafrika, im Südosten des Freistaates nahe der Grenze zu Lesotho, und zeichnet sich besonders durch seine malerischen Felslandschaften aus. Orange oder ocker gefärbte Sandsteinfelsen ragen über das bergige Grasland auf. Außerdem gibt es Felsmalereien der San.
Der nördliche Eingang zum Park liegt bei dem Künstlerdorf Clarens.
(Wikipedia)
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 paleontology finds have been made in the park, including dinosaur eggs and skeletons.
"Golden Gate" refers to the sandstone cliffs found on either side of the valley at the Golden Gate dam. In 1875, a farmer called J.N.R. van Reenen and his wife stopped here as they travelled to their new farm in Vuurland. He named the location "Golden Gate" when he saw the last rays of the setting sun fall on the cliffs.
In 1963, 47.92 km2 (11,840 acres) were proclaimed as a national park, specifically to preserve the scenic beauty of the area. In 1981, the park was enlarged to 62.41 km2 (15,420 acres), and in 1988, it was enlarged to 116.33 km2 (28,750 acres). In 2004, the park was announced to be joining with the neighbouring QwaQwa National Park. The amalgamation of QwaQwa National Park was completed in 2007, increasing the park's area to 340 km2 (84,000 acres).
The park is 320 km (200 mi) from Johannesburg and is close to the villages of Clarens and Kestell, in the upper regions of the Little Caledon River. The park is situated in the Rooiberge of the eastern Free State, in the foothills of the Maluti Mountains. The Caledon River forms the southern boundary of the park, as well as the border between the Free State and Lesotho. The highest peak in the park (and also in the Free State) is Ribbokkop at 2,829 m (9,281 ft) above sea level.
The park is located in the eastern highveld region of South Africa, and experiences a dry, sunny climate from June to August. It has showers, hail, and thunderstorms between October and April. It has thick snowfalls in the winter. The park has a relatively high rainfall of 800 mm (31 in) per year.
The park is an area of rich highveld and montane grassland flora. It has more than 60 grass species and a large variety of bulbs and herbs. Each of these species has its own flowering time, meaning that veld flowers can be seen throughout the summer. The park also has Afromontane forests and high-altitude Austro-Afro alpine grassland, which is scarce in South Africa. The ouhout (Leucosidea sericea), an evergreen species, is the most common tree in the park. Ouhout is a favourite habitat of beetles and 117 species occur on these trees in the park. The Lombardi poplars and weeping willows in the park are introduced species, but are kept because of their cultural and historic connection with the eastern Free State. Other exotic species in the park, for example wattle and bluegum, are systematically eradicated.
Instead of reintroducing one of the "big five" into the park, the sungazer lizard and water mongoose were reintroduced. Twelve species of mice, 10 species of carnivores, and 10 antelope species have been recorded in the park. The grey rhebuck and the mountain reedbuck were present when the park was established.
The geology of the park provides very visual "textbook" examples of Southern Africa's geological history. The sandstone formations in the park form the upper part of the Karoo Supergroup. These formations were deposited during a period of aeolian deposition towards the end of the Triassic Period. At the time of deposition, the climate of the area the park covers was becoming progressively drier until arid desert conditions set in, resulting in a land of dunes and sandy desert, with occasional scattered oases. The deposition of the sandstones ended when lava flowed out over the desert 190 million years ago.
The following sequence of geological formations is visible in the park (starting from the bottom): the Molteno Formation, Elliott Formation, Clarens Formation, and Drakensberg Formation. The yellow-brown Golden Gate and Brandwag cliffs are made up of the Clarens formation. The layers in this formation are 140 to 160 m (460 to 520 ft) thick. The Drakensberg formation comprises the basaltic lava that flowed over the desert. It forms the mountain summits in the park. On Ribbokkop, it is 600 m (2,000 ft) thick. The Elliot Formation is a red mudstone where many dinosaur fossils have been found.
The oldest dinosaur embryos ever discovered were found in the park in 1978. The eggs were from the Triassic Period (220 to 195 million years ago) and had fossilised foetal skeletons of Massospondylus, a prosauropod dinosaur. More examples of these eggs have since been found in the park. Other fossils found in the park include those of advanced cynodontia (canine toothed animals), small thecodontia (animals with teeth set firmly in the jaw), and bird-like and crocodile-like dinosaurs.
Accommodation in the park is available at Glen Reenen and Brandwag Rest camps. Caravan and camp sites with all amenities are available at Glen Reenen camp. The hotel was formerly part of Brandwag camp, but since its recent refurbishment, it is managed separately by SANParks as Golden Gate Hotel. The nearest town to Golden Gate Highlands National Park is Clarens (17 km to the west), but Phuthaditjhaba is also easily reached by a good tar road, driving through the access gate to the east of the park.
This park will be included into the Maloti-Drakensberg Transfrontier Conservation Area, Peace Park.
(Wikipedia)
Der Golden-Gate-Highlands-Nationalpark (englisch Golden Gate Highlands National Park) liegt in Südafrika, im Südosten des Freistaates nahe der Grenze zu Lesotho, und zeichnet sich besonders durch seine malerischen Felslandschaften aus. Orange oder ocker gefärbte Sandsteinfelsen ragen über das bergige Grasland auf. Außerdem gibt es Felsmalereien der San.
Der nördliche Eingang zum Park liegt bei dem Künstlerdorf Clarens.
(Wikipedia)
Blue Hour before Sunrise
Amphitheatre with the Eastern Buttress (3,047 m) seen from Upper Thendele Camp
Blaue Stunde vor Sonnenaufgang
Amphitheater mit dem Eastern Buttress (3.047 m) vom Upper Thendele Camp aus gesehen
The uKhahlamba-Drakensberg Park is in the KwaZulu-Natal province of South Africa, covering 2,428.13 km2 (938 sq mi) of area. The park includes Royal Natal National Park, a provincial park, and covers part of the Drakensberg, the highest mountain range in Southern Africa.
The park and the adjoining Sehlabathebe National Park in the Kingdom of Lesotho are part of the Maloti-Drakensberg Park, which was first declared a World Heritage Site on 30 November 2000. It is described by UNESCO as having "exceptional natural beauty in its soaring basaltic buttresses, incisive dramatic cutbacks, and golden sandstone ramparts... the site’s diversity of habitats protects a high level of endemic and globally threatened species, especially birds and plants... [and it] also contains many caves and rock-shelters with the largest and most concentrated group of paintings in Africa south of the Sahara".
Plans to boost tourism in the area include a long-awaited cable car project by the KZN Economic Development, Tourism and Environmental Affairs Department.
The Drakensberg mountain range is characterized by a high level of endemism of both invertebrates and vertebrates.
Most of the higher South African parts of the Drakensberg mountain range have been designated as game reserves or wilderness areas. The uKhahlamba-Drakensberg Park is also in the List of Wetlands of International Importance (under the Ramsar Convention). Adjacent to the park is the Cathkin Estates Conservation and Wildlife Sanctuary, which spans 1,044 ha (10 km2) of virgin grassland and represents the largest privately owned game park in the KwaZulu-Natal Drakensberg region.
(Wikipedia)
The Royal Natal National Park is in the KwaZulu Natal province of South Africa and forms part of the uKhahlamba Drakensberg Park World Heritage Site. Notwithstanding the name, it is actually not a South African National Park managed by the SANParks, but rather a Provincial Park managed by Ezemvelo KZN Wildlife. This park is now included into the Maloti-Drakensberg Transfrontier Conservation Area Peace Park.
The main features of the park are the Drakensberg Amphitheatre, a rock wall 5 kilometres (3.1 mi) long by up to 1,200 metres (3,900 ft) high, Mont-Aux-Sources peak where the Orange and Tugela rivers have their source, and the 948-metre (3,110 ft) Tugela Falls, the world's second-highest waterfall.
(Wikipedia)
Der uKhahlamba-Drakensberg Park (isiZulu uKhahlamba = „Barriere aus Speeren“) ist ein Nationalpark in den Drakensbergen in Südafrika. Im November 2000 wurde der Park in die UNESCO-Welterbe-Liste eingetragen. Der Park wird von der Provinzbehörde Ezemvelo KZN Wildlife verwaltet.
Der Park bedeckt eine Fläche von 2428 km². Er liegt in der Provinz KwaZulu-Natal und bildet einen 180 Kilometer langen und bis zu 20 Kilometer breiten Streifen entlang der Grenze zum Königreich Lesotho. Weitere Bestandteile des uKhahlamba-Drakensberg Park sind die getrennt liegenden Gebiete Royal-Natal-Nationalpark und Spioenkop Dam Nature Reserve weiter im Norden.
Der Park verfügt über hochaufragende Bergformationen und ist mit einem gut ausgebauten Netz von Wanderpfaden durchzogen. Basaltene, senkrecht aufragende Bergpfeiler, Bastionen aus goldbraunem Sandstein sowie skulpturierte Bögen, Höhlen, Säulen und Felswannen prägen das Landschaftsbild. Die Kette der Drakensberge im uKhahlamba-Drakensberg Park umfasst mehrere über 3000 Meter hohe Gipfel wie den Mafadi, den Giant’s Castle, den Cathedral Peak, den Monk’s Cowl, den Champagne Castle und den Njesuthi. Die Berghänge sind teilweise als Naturschutzgebiete ausgewiesen, in denen sich rund 30.000 Felsmalereien in etwa 600 Höhlen finden, die von San-Menschen über einen Zeitraum von 4000 Jahren erstellt wurden. In dieser Region entspringen die meisten großen Flüsse der Provinz KwaZulu-Natal. Sie bilden tiefe Schluchten und Täler. Einzige Straßenverbindung durch den Park nach Lesotho ist die Strecke über den Sanipass.
Es gibt eine Vielfalt endemischer Pflanzenarten, darunter Zuckerbüsche. Im Frühjahr übersäen in den Niederungen Teppiche von Wildblumen den Park, darunter Watsonia-Arten.
Zu den Vogelarten gehören Kapgeier (Gyps coprotheres) und Bartgeier (Gypaetus barbatus). Zahlreiche im Park beheimatete Wirbeltiere und Wirbellose sind endemisch. Weiterhin leben im Park Buschböcke, Ducker, Elenantilopen und Paviane.
1903 beschloss die Regierung der Kolonie Natal die Errichtung eines Naturschutzgebietes in den Drakensbergen. 1905 wurde eine klare Grenzziehung des Schutzbereichs proklamiert. 1916 wurde der Royal Natal National Park eingerichtet. Ab den 1950er Jahren wurden in den Drakensbergen diverse Naturschutzgebiete ausgewiesen, so 1951 das Kamberg Nature Reserve, 1953 das Nature Reserve de Lotheni und 1967 Vergelegen. Dabei wurde der Gewässerschutz vorangetrieben. 1973 kamen die Schutzgebiete Mdedelelo und Mkomazi hinzu.
Im Juni 2001 wurde des Maloti-Drakensberg Transfrontier Conservation Area (etwa: Maloti-Drakensberge-Grenzüberschreitendes-Erhaltungsgebiet) gegründet. Dieses verbindet den ukhahlamba-Drakensberg Park mit dem Sehlabathebe-Nationalpark in Lesotho. Ihm liegt der Anspruch an einen Peace Park (Transfrontier Conservation Area/TFCA) zugrunde. Die zwölf Kilometer lange Staatsgrenze kann zu Fuß passiert werden. Seit 2013 sind beide Nationalparks zusammen als Maloti Drakensberg Transboundary World Heritage Site in der UNESCO-Welterbe-Liste verzeichnet. Der gesamte Park ist nunmehr 2493 km² groß, wobei 65 km² der Fläche auf das Terrain Lesothos entfallen.
„… exceptional natural beauty in its soaring basaltic buttresses, incisive dramatic cutbacks, and golden sandstone ramparts … the site’s diversity of habitats protects a high level of endemic and globally threatened species, especially birds and plants … [and it] also contains many caves and rock-shelters with the largest and most concentrated group of paintings in Africa south of the Sahara. – … außergewöhnliche Schönheit der Natur in seinen aufragenden Basaltpfeilern, prägnante dramatische Einschnitte, und goldene Sandstein-Wälle … Die Vielfalt der Lebensräume beschützt ein hohes Maß an endemischen und vom Aussterben bedrohten Arten, vor allem Vögel und Pflanzen … [und es] enthält viele Höhlen und Felsnischen mit der größten und dichtesten Gruppe von Gemälden in Afrika südlich der Sahara.“
– Beschreibung des Maloti-Drakensberg Transfrontier Conservation Area auf der Website der UNESCO: Begründung zur Auswahl 2013
Teile der Drakensberg-Gebirgskette sind zu Schutzzwecken mit übergeordneter Bedeutung als Totalreservate ausgewiesen, sowie für touristische Zwecke daneben als Wildreservate. Entsprechend der Ramsar-Konvention wird der uKhahlamba Drakensberg Park auch als Schutzgut der List of Ramsar wetlands of international importance geführt. Private Eigentumsrechte hält an kleineren Gebietsteilen die Cathkin Estates Conservation and Wildlife Sanctuary.
(Wikipedia)
Der Royal Natal National Park wurde 1916 in den südafrikanischen Drakensbergen in der heutigen Provinz KwaZulu-Natal gebildet. Er ist Teil des Ukhahlamba-Drakensberg Park, der zum UNESCO-Welterbe gehört. Er gehört zu den spektakulärsten Natursehenswürdigkeiten in Afrika. Beeindruckend ist das Amphitheatre, eine mehrere Kilometer lange und etwa 1000 Meter hohe Felswand zwischen Sentinel (3165 m) und Eastern Buttress (3047 m). Auf dem flachen Gipfelplateau stehen einige Berge wie der Mont-Aux-Sources (Sesotho: Phofung) (3282 m), den 1836 die französischen Missionare Thomas Arbousset und François Daumas bestiegen und nach den Quellen von drei größeren Flüssen benannten.
Einer von diesen, der Tugela, stürzt in den Tugelafällen in fünf Stufen 948 Meter in die Tiefe (andere Angaben: knapp 3000 Fuß, 540 m). In kalten Wintern friert er in den oberen Stufen und bildet eindrucksvolle Eissäulen.
Der Royal Natal National Park ist ideal geeignet für Wanderungen mit einem Netz von klassifizierten Wegen aller Schwierigkeitsgrade; dies reicht von der leichten Besteigung des Mont-aux-Sources vom Plateau aus bis zur jährlichen Mont-aux-Sources Challenge, wenn Querfeldeinläufer zusammenkommen, um die 50 Kilometer lange Strecke in weniger als fünf Stunden zu absolvieren.
(Wikipedia)
Hike around Plowman's Kop via the Crack and Mudslide.
Wanderung über den Plowman's Kop über Crack und Mudslide.
The uKhahlamba-Drakensberg Park is in the KwaZulu-Natal province of South Africa, covering 2,428.13 km2 (938 sq mi) of area. The park includes Royal Natal National Park, a provincial park, and covers part of the Drakensberg, the highest mountain range in Southern Africa.
The park and the adjoining Sehlabathebe National Park in the Kingdom of Lesotho are part of the Maloti-Drakensberg Park, which was first declared a World Heritage Site on 30 November 2000. It is described by UNESCO as having "exceptional natural beauty in its soaring basaltic buttresses, incisive dramatic cutbacks, and golden sandstone ramparts... the site’s diversity of habitats protects a high level of endemic and globally threatened species, especially birds and plants... [and it] also contains many caves and rock-shelters with the largest and most concentrated group of paintings in Africa south of the Sahara".
Plans to boost tourism in the area include a long-awaited cable car project by the KZN Economic Development, Tourism and Environmental Affairs Department.
The Drakensberg mountain range is characterized by a high level of endemism of both invertebrates and vertebrates.
Most of the higher South African parts of the Drakensberg mountain range have been designated as game reserves or wilderness areas. The uKhahlamba-Drakensberg Park is also in the List of Wetlands of International Importance (under the Ramsar Convention). Adjacent to the park is the Cathkin Estates Conservation and Wildlife Sanctuary, which spans 1,044 ha (10 km2) of virgin grassland and represents the largest privately owned game park in the KwaZulu-Natal Drakensberg region.
(Wikipedia)
The Royal Natal National Park is in the KwaZulu Natal province of South Africa and forms part of the uKhahlamba Drakensberg Park World Heritage Site. Notwithstanding the name, it is actually not a South African National Park managed by the SANParks, but rather a Provincial Park managed by Ezemvelo KZN Wildlife. This park is now included into the Maloti-Drakensberg Transfrontier Conservation Area Peace Park.
The main features of the park are the Drakensberg Amphitheatre, a rock wall 5 kilometres (3.1 mi) long by up to 1,200 metres (3,900 ft) high, Mont-Aux-Sources peak where the Orange and Tugela rivers have their source, and the 948-metre (3,110 ft) Tugela Falls, the world's second-highest waterfall.
(Wikipedia)
Der uKhahlamba-Drakensberg Park (isiZulu uKhahlamba = „Barriere aus Speeren“) ist ein Nationalpark in den Drakensbergen in Südafrika. Im November 2000 wurde der Park in die UNESCO-Welterbe-Liste eingetragen. Der Park wird von der Provinzbehörde Ezemvelo KZN Wildlife verwaltet.
Der Park bedeckt eine Fläche von 2428 km². Er liegt in der Provinz KwaZulu-Natal und bildet einen 180 Kilometer langen und bis zu 20 Kilometer breiten Streifen entlang der Grenze zum Königreich Lesotho. Weitere Bestandteile des uKhahlamba-Drakensberg Park sind die getrennt liegenden Gebiete Royal-Natal-Nationalpark und Spioenkop Dam Nature Reserve weiter im Norden.
Der Park verfügt über hochaufragende Bergformationen und ist mit einem gut ausgebauten Netz von Wanderpfaden durchzogen. Basaltene, senkrecht aufragende Bergpfeiler, Bastionen aus goldbraunem Sandstein sowie skulpturierte Bögen, Höhlen, Säulen und Felswannen prägen das Landschaftsbild. Die Kette der Drakensberge im uKhahlamba-Drakensberg Park umfasst mehrere über 3000 Meter hohe Gipfel wie den Mafadi, den Giant’s Castle, den Cathedral Peak, den Monk’s Cowl, den Champagne Castle und den Njesuthi. Die Berghänge sind teilweise als Naturschutzgebiete ausgewiesen, in denen sich rund 30.000 Felsmalereien in etwa 600 Höhlen finden, die von San-Menschen über einen Zeitraum von 4000 Jahren erstellt wurden. In dieser Region entspringen die meisten großen Flüsse der Provinz KwaZulu-Natal. Sie bilden tiefe Schluchten und Täler. Einzige Straßenverbindung durch den Park nach Lesotho ist die Strecke über den Sanipass.
Es gibt eine Vielfalt endemischer Pflanzenarten, darunter Zuckerbüsche. Im Frühjahr übersäen in den Niederungen Teppiche von Wildblumen den Park, darunter Watsonia-Arten.
Zu den Vogelarten gehören Kapgeier (Gyps coprotheres) und Bartgeier (Gypaetus barbatus). Zahlreiche im Park beheimatete Wirbeltiere und Wirbellose sind endemisch. Weiterhin leben im Park Buschböcke, Ducker, Elenantilopen und Paviane.
1903 beschloss die Regierung der Kolonie Natal die Errichtung eines Naturschutzgebietes in den Drakensbergen. 1905 wurde eine klare Grenzziehung des Schutzbereichs proklamiert. 1916 wurde der Royal Natal National Park eingerichtet. Ab den 1950er Jahren wurden in den Drakensbergen diverse Naturschutzgebiete ausgewiesen, so 1951 das Kamberg Nature Reserve, 1953 das Nature Reserve de Lotheni und 1967 Vergelegen. Dabei wurde der Gewässerschutz vorangetrieben. 1973 kamen die Schutzgebiete Mdedelelo und Mkomazi hinzu.
Im Juni 2001 wurde des Maloti-Drakensberg Transfrontier Conservation Area (etwa: Maloti-Drakensberge-Grenzüberschreitendes-Erhaltungsgebiet) gegründet. Dieses verbindet den ukhahlamba-Drakensberg Park mit dem Sehlabathebe-Nationalpark in Lesotho. Ihm liegt der Anspruch an einen Peace Park (Transfrontier Conservation Area/TFCA) zugrunde. Die zwölf Kilometer lange Staatsgrenze kann zu Fuß passiert werden. Seit 2013 sind beide Nationalparks zusammen als Maloti Drakensberg Transboundary World Heritage Site in der UNESCO-Welterbe-Liste verzeichnet. Der gesamte Park ist nunmehr 2493 km² groß, wobei 65 km² der Fläche auf das Terrain Lesothos entfallen.
„… exceptional natural beauty in its soaring basaltic buttresses, incisive dramatic cutbacks, and golden sandstone ramparts … the site’s diversity of habitats protects a high level of endemic and globally threatened species, especially birds and plants … [and it] also contains many caves and rock-shelters with the largest and most concentrated group of paintings in Africa south of the Sahara. – … außergewöhnliche Schönheit der Natur in seinen aufragenden Basaltpfeilern, prägnante dramatische Einschnitte, und goldene Sandstein-Wälle … Die Vielfalt der Lebensräume beschützt ein hohes Maß an endemischen und vom Aussterben bedrohten Arten, vor allem Vögel und Pflanzen … [und es] enthält viele Höhlen und Felsnischen mit der größten und dichtesten Gruppe von Gemälden in Afrika südlich der Sahara.“
– Beschreibung des Maloti-Drakensberg Transfrontier Conservation Area auf der Website der UNESCO: Begründung zur Auswahl 2013
Teile der Drakensberg-Gebirgskette sind zu Schutzzwecken mit übergeordneter Bedeutung als Totalreservate ausgewiesen, sowie für touristische Zwecke daneben als Wildreservate. Entsprechend der Ramsar-Konvention wird der uKhahlamba Drakensberg Park auch als Schutzgut der List of Ramsar wetlands of international importance geführt. Private Eigentumsrechte hält an kleineren Gebietsteilen die Cathkin Estates Conservation and Wildlife Sanctuary.
(Wikipedia)
Der Royal Natal National Park wurde 1916 in den südafrikanischen Drakensbergen in der heutigen Provinz KwaZulu-Natal gebildet. Er ist Teil des Ukhahlamba-Drakensberg Park, der zum UNESCO-Welterbe gehört. Er gehört zu den spektakulärsten Natursehenswürdigkeiten in Afrika. Beeindruckend ist das Amphitheatre, eine mehrere Kilometer lange und etwa 1000 Meter hohe Felswand zwischen Sentinel (3165 m) und Eastern Buttress (3047 m). Auf dem flachen Gipfelplateau stehen einige Berge wie der Mont-Aux-Sources (Sesotho: Phofung) (3282 m), den 1836 die französischen Missionare Thomas Arbousset und François Daumas bestiegen und nach den Quellen von drei größeren Flüssen benannten.
Einer von diesen, der Tugela, stürzt in den Tugelafällen in fünf Stufen 948 Meter in die Tiefe (andere Angaben: knapp 3000 Fuß, 540 m). In kalten Wintern friert er in den oberen Stufen und bildet eindrucksvolle Eissäulen.
Der Royal Natal National Park ist ideal geeignet für Wanderungen mit einem Netz von klassifizierten Wegen aller Schwierigkeitsgrade; dies reicht von der leichten Besteigung des Mont-aux-Sources vom Plateau aus bis zur jährlichen Mont-aux-Sources Challenge, wenn Querfeldeinläufer zusammenkommen, um die 50 Kilometer lange Strecke in weniger als fünf Stunden zu absolvieren.
(Wikipedia)
Blesboks
Blesboks
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 paleontology finds have been made in the park, including dinosaur eggs and skeletons.
"Golden Gate" refers to the sandstone cliffs found on either side of the valley at the Golden Gate dam. In 1875, a farmer called J.N.R. van Reenen and his wife stopped here as they travelled to their new farm in Vuurland. He named the location "Golden Gate" when he saw the last rays of the setting sun fall on the cliffs.
In 1963, 47.92 km2 (11,840 acres) were proclaimed as a national park, specifically to preserve the scenic beauty of the area. In 1981, the park was enlarged to 62.41 km2 (15,420 acres), and in 1988, it was enlarged to 116.33 km2 (28,750 acres). In 2004, the park was announced to be joining with the neighbouring QwaQwa National Park. The amalgamation of QwaQwa National Park was completed in 2007, increasing the park's area to 340 km2 (84,000 acres).
The park is 320 km (200 mi) from Johannesburg and is close to the villages of Clarens and Kestell, in the upper regions of the Little Caledon River. The park is situated in the Rooiberge of the eastern Free State, in the foothills of the Maluti Mountains. The Caledon River forms the southern boundary of the park, as well as the border between the Free State and Lesotho. The highest peak in the park (and also in the Free State) is Ribbokkop at 2,829 m (9,281 ft) above sea level.
The park is located in the eastern highveld region of South Africa, and experiences a dry, sunny climate from June to August. It has showers, hail, and thunderstorms between October and April. It has thick snowfalls in the winter. The park has a relatively high rainfall of 800 mm (31 in) per year.
The park is an area of rich highveld and montane grassland flora. It has more than 60 grass species and a large variety of bulbs and herbs. Each of these species has its own flowering time, meaning that veld flowers can be seen throughout the summer. The park also has Afromontane forests and high-altitude Austro-Afro alpine grassland, which is scarce in South Africa. The ouhout (Leucosidea sericea), an evergreen species, is the most common tree in the park. Ouhout is a favourite habitat of beetles and 117 species occur on these trees in the park. The Lombardi poplars and weeping willows in the park are introduced species, but are kept because of their cultural and historic connection with the eastern Free State. Other exotic species in the park, for example wattle and bluegum, are systematically eradicated.
Instead of reintroducing one of the "big five" into the park, the sungazer lizard and water mongoose were reintroduced. Twelve species of mice, 10 species of carnivores, and 10 antelope species have been recorded in the park. The grey rhebuck and the mountain reedbuck were present when the park was established.
The geology of the park provides very visual "textbook" examples of Southern Africa's geological history. The sandstone formations in the park form the upper part of the Karoo Supergroup. These formations were deposited during a period of aeolian deposition towards the end of the Triassic Period. At the time of deposition, the climate of the area the park covers was becoming progressively drier until arid desert conditions set in, resulting in a land of dunes and sandy desert, with occasional scattered oases. The deposition of the sandstones ended when lava flowed out over the desert 190 million years ago.
The following sequence of geological formations is visible in the park (starting from the bottom): the Molteno Formation, Elliott Formation, Clarens Formation, and Drakensberg Formation. The yellow-brown Golden Gate and Brandwag cliffs are made up of the Clarens formation. The layers in this formation are 140 to 160 m (460 to 520 ft) thick. The Drakensberg formation comprises the basaltic lava that flowed over the desert. It forms the mountain summits in the park. On Ribbokkop, it is 600 m (2,000 ft) thick. The Elliot Formation is a red mudstone where many dinosaur fossils have been found.
The oldest dinosaur embryos ever discovered were found in the park in 1978. The eggs were from the Triassic Period (220 to 195 million years ago) and had fossilised foetal skeletons of Massospondylus, a prosauropod dinosaur. More examples of these eggs have since been found in the park. Other fossils found in the park include those of advanced cynodontia (canine toothed animals), small thecodontia (animals with teeth set firmly in the jaw), and bird-like and crocodile-like dinosaurs.
Accommodation in the park is available at Glen Reenen and Brandwag Rest camps. Caravan and camp sites with all amenities are available at Glen Reenen camp. The hotel was formerly part of Brandwag camp, but since its recent refurbishment, it is managed separately by SANParks as Golden Gate Hotel. The nearest town to Golden Gate Highlands National Park is Clarens (17 km to the west), but Phuthaditjhaba is also easily reached by a good tar road, driving through the access gate to the east of the park.
This park will be included into the Maloti-Drakensberg Transfrontier Conservation Area, Peace Park.
(Wikipedia)
The blesbok or blesbuck (Damaliscus pygargus phillipsi) is an antelope endemic to South Africa. It has a distinctive white face and forehead which inspired the name, because bles is the Afrikaans word for a blaze such as one might see on the forehead of a horse.
The blesbok and the bontebok (Damaliscus pygargus dorcas) are variant subspecies of one another and can readily interbreed, the offspring being known as the bontebles or baster blesbok, the differences between the two subspecies have arisen due to preferences for different habitats in the wild. The blesbok is endemic to southern Africa and is found in large numbers in all national parks with open grasslands, from the Highveld north of the Vaal river southwards through the Free State, to the Eastern Cape. It is a plains species and dislikes wooded areas. It was first discovered in the 17th century, in numbers so numerous, herds reached from horizon to horizon.
Physically, rams and ewes are remarkably similar. Their mass can be as much as 85 kg. A characteristic of the blesbok is the prominent white blaze on the face and a horizontal brown strip which divides this blaze above the eyes. Body colour is brown with a lighter-coloured saddle on the back, and the rump an even lighter shade. The legs are brown with a white patch behind the top part of the front legs. Lower legs whitish. Both sexes carry horns, ringed almost to the tip. Female horns are slightly more slender. The neck and the top of the back of the blesbok is brown. Lower down on the flanks and buttocks, the coloring becomes darker. The belly, the inside of the buttocks and the area up to the base of the tail is white. Blesbok can be easily differentiated from other antelopes because they have a distinct white face and forehead. The blesbok differs from the bontebok by having less white on the coat and the blaze on the face, which is usually divided, the coat is also a lighter yellow than that of the bontebok. The length of their horns averages at around 38 cm. Male adult blesbok average around 70 kg; females average lower, at around 61 kg.
Body length: 140–160 cm (4.6–5.2 ft)
Shoulder height: 85–100 cm (2.79–3.28 ft)
Tail length: 30–45 cm (12–18 in)
Weight: 55–80 kg (121–176 lb)
Blesbok can be found in open veld or plains of South Africa and Namibia. Their preferred habitat is open grassland with water. They often occupy relatively small territories of 2.5 to 6.0 acres in size. They were once one of the most abundant antelope species of the African plains, but have become scarce since 1893 due to relentless hunting for their skins and meat.
The blesbok is a seasonal breeder, with rutting from March to May. Births peak during November and December after a gestation period of about 240 days (8 months). Females give birth to a single calf per breeding season.
The blesbok was hunted nearly to extinction because of its large numbers, but having been protected since the late 19th century, it has proliferated and today it is sufficiently numerous not to be classed as endangered. In modern times, this is largely because of the commercial value of the blesbok to private land owners, and also because it is one of the few medium-sized antelope that can be contained by normal stock fencing. At the start of the 21st century, blesbok numbers are stable, estimated to be around 240,000. However, 97% of them live outside reserves, and only 3% in national parks. They also are common in zoos, though in far smaller numbers.
Humans, lions, leopards, African wild dogs, spotted hyenas, and cheetahs are the blesbok's main predators, while jackals and eagles may attack the calves. The blesbok is both farmed and hunted for the skin, meat, and trophy. Blesbok are shy and alert; they rely on speed and endurance to escape predators, but have an tendency to return to place where they were attacked after a few minutes. They can maintain a speed of 70 km/h (43 mph) when chased, but, like other white-fronted damalisques, blesbok are not good jumpers or crawlers.
Fossil remains of a prehistoric relative, Damaliscus niro, were found in deposits in Sterkfontein. With a weight of approximately 120 kg, it was heavier than the modern blesbok and it had slightly different horns. D. niro became extinct at the end of the Pleistocene 12 thousand years ago.
(Wikipedia)
Der Golden-Gate-Highlands-Nationalpark (englisch Golden Gate Highlands National Park) liegt in Südafrika, im Südosten des Freistaates nahe der Grenze zu Lesotho, und zeichnet sich besonders durch seine malerischen Felslandschaften aus. Orange oder ocker gefärbte Sandsteinfelsen ragen über das bergige Grasland auf. Außerdem gibt es Felsmalereien der San.
Der nördliche Eingang zum Park liegt bei dem Künstlerdorf Clarens.
(Wikipedia)
Thukela Gorge Hike
Wanderung in die Thukela Schlucht
Policeman's Helmet
The uKhahlamba-Drakensberg Park is in the KwaZulu-Natal province of South Africa, covering 2,428.13 km2 (938 sq mi) of area. The park includes Royal Natal National Park, a provincial park, and covers part of the Drakensberg, the highest mountain range in Southern Africa.
The park and the adjoining Sehlabathebe National Park in the Kingdom of Lesotho are part of the Maloti-Drakensberg Park, which was first declared a World Heritage Site on 30 November 2000. It is described by UNESCO as having "exceptional natural beauty in its soaring basaltic buttresses, incisive dramatic cutbacks, and golden sandstone ramparts... the site’s diversity of habitats protects a high level of endemic and globally threatened species, especially birds and plants... [and it] also contains many caves and rock-shelters with the largest and most concentrated group of paintings in Africa south of the Sahara".
Plans to boost tourism in the area include a long-awaited cable car project by the KZN Economic Development, Tourism and Environmental Affairs Department.
The Drakensberg mountain range is characterized by a high level of endemism of both invertebrates and vertebrates.
Most of the higher South African parts of the Drakensberg mountain range have been designated as game reserves or wilderness areas. The uKhahlamba-Drakensberg Park is also in the List of Wetlands of International Importance (under the Ramsar Convention). Adjacent to the park is the Cathkin Estates Conservation and Wildlife Sanctuary, which spans 1,044 ha (10 km2) of virgin grassland and represents the largest privately owned game park in the KwaZulu-Natal Drakensberg region.
(Wikipedia)
The Royal Natal National Park is in the KwaZulu Natal province of South Africa and forms part of the uKhahlamba Drakensberg Park World Heritage Site. Notwithstanding the name, it is actually not a South African National Park managed by the SANParks, but rather a Provincial Park managed by Ezemvelo KZN Wildlife. This park is now included into the Maloti-Drakensberg Transfrontier Conservation Area Peace Park.
The main features of the park are the Drakensberg Amphitheatre, a rock wall 5 kilometres (3.1 mi) long by up to 1,200 metres (3,900 ft) high, Mont-Aux-Sources peak where the Orange and Tugela rivers have their source, and the 948-metre (3,110 ft) Tugela Falls, the world's second-highest waterfall.
(Wikipedia)
Der uKhahlamba-Drakensberg Park (isiZulu uKhahlamba = „Barriere aus Speeren“) ist ein Nationalpark in den Drakensbergen in Südafrika. Im November 2000 wurde der Park in die UNESCO-Welterbe-Liste eingetragen. Der Park wird von der Provinzbehörde Ezemvelo KZN Wildlife verwaltet.
Der Park bedeckt eine Fläche von 2428 km². Er liegt in der Provinz KwaZulu-Natal und bildet einen 180 Kilometer langen und bis zu 20 Kilometer breiten Streifen entlang der Grenze zum Königreich Lesotho. Weitere Bestandteile des uKhahlamba-Drakensberg Park sind die getrennt liegenden Gebiete Royal-Natal-Nationalpark und Spioenkop Dam Nature Reserve weiter im Norden.
Der Park verfügt über hochaufragende Bergformationen und ist mit einem gut ausgebauten Netz von Wanderpfaden durchzogen. Basaltene, senkrecht aufragende Bergpfeiler, Bastionen aus goldbraunem Sandstein sowie skulpturierte Bögen, Höhlen, Säulen und Felswannen prägen das Landschaftsbild. Die Kette der Drakensberge im uKhahlamba-Drakensberg Park umfasst mehrere über 3000 Meter hohe Gipfel wie den Mafadi, den Giant’s Castle, den Cathedral Peak, den Monk’s Cowl, den Champagne Castle und den Njesuthi. Die Berghänge sind teilweise als Naturschutzgebiete ausgewiesen, in denen sich rund 30.000 Felsmalereien in etwa 600 Höhlen finden, die von San-Menschen über einen Zeitraum von 4000 Jahren erstellt wurden. In dieser Region entspringen die meisten großen Flüsse der Provinz KwaZulu-Natal. Sie bilden tiefe Schluchten und Täler. Einzige Straßenverbindung durch den Park nach Lesotho ist die Strecke über den Sanipass.
Es gibt eine Vielfalt endemischer Pflanzenarten, darunter Zuckerbüsche. Im Frühjahr übersäen in den Niederungen Teppiche von Wildblumen den Park, darunter Watsonia-Arten.
Zu den Vogelarten gehören Kapgeier (Gyps coprotheres) und Bartgeier (Gypaetus barbatus). Zahlreiche im Park beheimatete Wirbeltiere und Wirbellose sind endemisch. Weiterhin leben im Park Buschböcke, Ducker, Elenantilopen und Paviane.
1903 beschloss die Regierung der Kolonie Natal die Errichtung eines Naturschutzgebietes in den Drakensbergen. 1905 wurde eine klare Grenzziehung des Schutzbereichs proklamiert. 1916 wurde der Royal Natal National Park eingerichtet. Ab den 1950er Jahren wurden in den Drakensbergen diverse Naturschutzgebiete ausgewiesen, so 1951 das Kamberg Nature Reserve, 1953 das Nature Reserve de Lotheni und 1967 Vergelegen. Dabei wurde der Gewässerschutz vorangetrieben. 1973 kamen die Schutzgebiete Mdedelelo und Mkomazi hinzu.
Im Juni 2001 wurde des Maloti-Drakensberg Transfrontier Conservation Area (etwa: Maloti-Drakensberge-Grenzüberschreitendes-Erhaltungsgebiet) gegründet. Dieses verbindet den ukhahlamba-Drakensberg Park mit dem Sehlabathebe-Nationalpark in Lesotho. Ihm liegt der Anspruch an einen Peace Park (Transfrontier Conservation Area/TFCA) zugrunde. Die zwölf Kilometer lange Staatsgrenze kann zu Fuß passiert werden. Seit 2013 sind beide Nationalparks zusammen als Maloti Drakensberg Transboundary World Heritage Site in der UNESCO-Welterbe-Liste verzeichnet. Der gesamte Park ist nunmehr 2493 km² groß, wobei 65 km² der Fläche auf das Terrain Lesothos entfallen.
„… exceptional natural beauty in its soaring basaltic buttresses, incisive dramatic cutbacks, and golden sandstone ramparts … the site’s diversity of habitats protects a high level of endemic and globally threatened species, especially birds and plants … [and it] also contains many caves and rock-shelters with the largest and most concentrated group of paintings in Africa south of the Sahara. – … außergewöhnliche Schönheit der Natur in seinen aufragenden Basaltpfeilern, prägnante dramatische Einschnitte, und goldene Sandstein-Wälle … Die Vielfalt der Lebensräume beschützt ein hohes Maß an endemischen und vom Aussterben bedrohten Arten, vor allem Vögel und Pflanzen … [und es] enthält viele Höhlen und Felsnischen mit der größten und dichtesten Gruppe von Gemälden in Afrika südlich der Sahara.“
– Beschreibung des Maloti-Drakensberg Transfrontier Conservation Area auf der Website der UNESCO: Begründung zur Auswahl 2013
Teile der Drakensberg-Gebirgskette sind zu Schutzzwecken mit übergeordneter Bedeutung als Totalreservate ausgewiesen, sowie für touristische Zwecke daneben als Wildreservate. Entsprechend der Ramsar-Konvention wird der uKhahlamba Drakensberg Park auch als Schutzgut der List of Ramsar wetlands of international importance geführt. Private Eigentumsrechte hält an kleineren Gebietsteilen die Cathkin Estates Conservation and Wildlife Sanctuary.
(Wikipedia)
Der Royal Natal National Park wurde 1916 in den südafrikanischen Drakensbergen in der heutigen Provinz KwaZulu-Natal gebildet. Er ist Teil des Ukhahlamba-Drakensberg Park, der zum UNESCO-Welterbe gehört. Er gehört zu den spektakulärsten Natursehenswürdigkeiten in Afrika. Beeindruckend ist das Amphitheatre, eine mehrere Kilometer lange und etwa 1000 Meter hohe Felswand zwischen Sentinel (3165 m) und Eastern Buttress (3047 m). Auf dem flachen Gipfelplateau stehen einige Berge wie der Mont-Aux-Sources (Sesotho: Phofung) (3282 m), den 1836 die französischen Missionare Thomas Arbousset und François Daumas bestiegen und nach den Quellen von drei größeren Flüssen benannten.
Einer von diesen, der Tugela, stürzt in den Tugelafällen in fünf Stufen 948 Meter in die Tiefe (andere Angaben: knapp 3000 Fuß, 540 m). In kalten Wintern friert er in den oberen Stufen und bildet eindrucksvolle Eissäulen.
Der Royal Natal National Park ist ideal geeignet für Wanderungen mit einem Netz von klassifizierten Wegen aller Schwierigkeitsgrade; dies reicht von der leichten Besteigung des Mont-aux-Sources vom Plateau aus bis zur jährlichen Mont-aux-Sources Challenge, wenn Querfeldeinläufer zusammenkommen, um die 50 Kilometer lange Strecke in weniger als fünf Stunden zu absolvieren.
(Wikipedia)
Hike around Plowman's Kop via the Crack and Mudslide.
Wanderung über den Plowman's Kop über Crack und Mudslide.
The uKhahlamba-Drakensberg Park is in the KwaZulu-Natal province of South Africa, covering 2,428.13 km2 (938 sq mi) of area. The park includes Royal Natal National Park, a provincial park, and covers part of the Drakensberg, the highest mountain range in Southern Africa.
The park and the adjoining Sehlabathebe National Park in the Kingdom of Lesotho are part of the Maloti-Drakensberg Park, which was first declared a World Heritage Site on 30 November 2000. It is described by UNESCO as having "exceptional natural beauty in its soaring basaltic buttresses, incisive dramatic cutbacks, and golden sandstone ramparts... the site’s diversity of habitats protects a high level of endemic and globally threatened species, especially birds and plants... [and it] also contains many caves and rock-shelters with the largest and most concentrated group of paintings in Africa south of the Sahara".
Plans to boost tourism in the area include a long-awaited cable car project by the KZN Economic Development, Tourism and Environmental Affairs Department.
The Drakensberg mountain range is characterized by a high level of endemism of both invertebrates and vertebrates.
Most of the higher South African parts of the Drakensberg mountain range have been designated as game reserves or wilderness areas. The uKhahlamba-Drakensberg Park is also in the List of Wetlands of International Importance (under the Ramsar Convention). Adjacent to the park is the Cathkin Estates Conservation and Wildlife Sanctuary, which spans 1,044 ha (10 km2) of virgin grassland and represents the largest privately owned game park in the KwaZulu-Natal Drakensberg region.
(Wikipedia)
The Royal Natal National Park is in the KwaZulu Natal province of South Africa and forms part of the uKhahlamba Drakensberg Park World Heritage Site. Notwithstanding the name, it is actually not a South African National Park managed by the SANParks, but rather a Provincial Park managed by Ezemvelo KZN Wildlife. This park is now included into the Maloti-Drakensberg Transfrontier Conservation Area Peace Park.
The main features of the park are the Drakensberg Amphitheatre, a rock wall 5 kilometres (3.1 mi) long by up to 1,200 metres (3,900 ft) high, Mont-Aux-Sources peak where the Orange and Tugela rivers have their source, and the 948-metre (3,110 ft) Tugela Falls, the world's second-highest waterfall.
(Wikipedia)
Der uKhahlamba-Drakensberg Park (isiZulu uKhahlamba = „Barriere aus Speeren“) ist ein Nationalpark in den Drakensbergen in Südafrika. Im November 2000 wurde der Park in die UNESCO-Welterbe-Liste eingetragen. Der Park wird von der Provinzbehörde Ezemvelo KZN Wildlife verwaltet.
Der Park bedeckt eine Fläche von 2428 km². Er liegt in der Provinz KwaZulu-Natal und bildet einen 180 Kilometer langen und bis zu 20 Kilometer breiten Streifen entlang der Grenze zum Königreich Lesotho. Weitere Bestandteile des uKhahlamba-Drakensberg Park sind die getrennt liegenden Gebiete Royal-Natal-Nationalpark und Spioenkop Dam Nature Reserve weiter im Norden.
Der Park verfügt über hochaufragende Bergformationen und ist mit einem gut ausgebauten Netz von Wanderpfaden durchzogen. Basaltene, senkrecht aufragende Bergpfeiler, Bastionen aus goldbraunem Sandstein sowie skulpturierte Bögen, Höhlen, Säulen und Felswannen prägen das Landschaftsbild. Die Kette der Drakensberge im uKhahlamba-Drakensberg Park umfasst mehrere über 3000 Meter hohe Gipfel wie den Mafadi, den Giant’s Castle, den Cathedral Peak, den Monk’s Cowl, den Champagne Castle und den Njesuthi. Die Berghänge sind teilweise als Naturschutzgebiete ausgewiesen, in denen sich rund 30.000 Felsmalereien in etwa 600 Höhlen finden, die von San-Menschen über einen Zeitraum von 4000 Jahren erstellt wurden. In dieser Region entspringen die meisten großen Flüsse der Provinz KwaZulu-Natal. Sie bilden tiefe Schluchten und Täler. Einzige Straßenverbindung durch den Park nach Lesotho ist die Strecke über den Sanipass.
Es gibt eine Vielfalt endemischer Pflanzenarten, darunter Zuckerbüsche. Im Frühjahr übersäen in den Niederungen Teppiche von Wildblumen den Park, darunter Watsonia-Arten.
Zu den Vogelarten gehören Kapgeier (Gyps coprotheres) und Bartgeier (Gypaetus barbatus). Zahlreiche im Park beheimatete Wirbeltiere und Wirbellose sind endemisch. Weiterhin leben im Park Buschböcke, Ducker, Elenantilopen und Paviane.
1903 beschloss die Regierung der Kolonie Natal die Errichtung eines Naturschutzgebietes in den Drakensbergen. 1905 wurde eine klare Grenzziehung des Schutzbereichs proklamiert. 1916 wurde der Royal Natal National Park eingerichtet. Ab den 1950er Jahren wurden in den Drakensbergen diverse Naturschutzgebiete ausgewiesen, so 1951 das Kamberg Nature Reserve, 1953 das Nature Reserve de Lotheni und 1967 Vergelegen. Dabei wurde der Gewässerschutz vorangetrieben. 1973 kamen die Schutzgebiete Mdedelelo und Mkomazi hinzu.
Im Juni 2001 wurde des Maloti-Drakensberg Transfrontier Conservation Area (etwa: Maloti-Drakensberge-Grenzüberschreitendes-Erhaltungsgebiet) gegründet. Dieses verbindet den ukhahlamba-Drakensberg Park mit dem Sehlabathebe-Nationalpark in Lesotho. Ihm liegt der Anspruch an einen Peace Park (Transfrontier Conservation Area/TFCA) zugrunde. Die zwölf Kilometer lange Staatsgrenze kann zu Fuß passiert werden. Seit 2013 sind beide Nationalparks zusammen als Maloti Drakensberg Transboundary World Heritage Site in der UNESCO-Welterbe-Liste verzeichnet. Der gesamte Park ist nunmehr 2493 km² groß, wobei 65 km² der Fläche auf das Terrain Lesothos entfallen.
„… exceptional natural beauty in its soaring basaltic buttresses, incisive dramatic cutbacks, and golden sandstone ramparts … the site’s diversity of habitats protects a high level of endemic and globally threatened species, especially birds and plants … [and it] also contains many caves and rock-shelters with the largest and most concentrated group of paintings in Africa south of the Sahara. – … außergewöhnliche Schönheit der Natur in seinen aufragenden Basaltpfeilern, prägnante dramatische Einschnitte, und goldene Sandstein-Wälle … Die Vielfalt der Lebensräume beschützt ein hohes Maß an endemischen und vom Aussterben bedrohten Arten, vor allem Vögel und Pflanzen … [und es] enthält viele Höhlen und Felsnischen mit der größten und dichtesten Gruppe von Gemälden in Afrika südlich der Sahara.“
– Beschreibung des Maloti-Drakensberg Transfrontier Conservation Area auf der Website der UNESCO: Begründung zur Auswahl 2013
Teile der Drakensberg-Gebirgskette sind zu Schutzzwecken mit übergeordneter Bedeutung als Totalreservate ausgewiesen, sowie für touristische Zwecke daneben als Wildreservate. Entsprechend der Ramsar-Konvention wird der uKhahlamba Drakensberg Park auch als Schutzgut der List of Ramsar wetlands of international importance geführt. Private Eigentumsrechte hält an kleineren Gebietsteilen die Cathkin Estates Conservation and Wildlife Sanctuary.
(Wikipedia)
Der Royal Natal National Park wurde 1916 in den südafrikanischen Drakensbergen in der heutigen Provinz KwaZulu-Natal gebildet. Er ist Teil des Ukhahlamba-Drakensberg Park, der zum UNESCO-Welterbe gehört. Er gehört zu den spektakulärsten Natursehenswürdigkeiten in Afrika. Beeindruckend ist das Amphitheatre, eine mehrere Kilometer lange und etwa 1000 Meter hohe Felswand zwischen Sentinel (3165 m) und Eastern Buttress (3047 m). Auf dem flachen Gipfelplateau stehen einige Berge wie der Mont-Aux-Sources (Sesotho: Phofung) (3282 m), den 1836 die französischen Missionare Thomas Arbousset und François Daumas bestiegen und nach den Quellen von drei größeren Flüssen benannten.
Einer von diesen, der Tugela, stürzt in den Tugelafällen in fünf Stufen 948 Meter in die Tiefe (andere Angaben: knapp 3000 Fuß, 540 m). In kalten Wintern friert er in den oberen Stufen und bildet eindrucksvolle Eissäulen.
Der Royal Natal National Park ist ideal geeignet für Wanderungen mit einem Netz von klassifizierten Wegen aller Schwierigkeitsgrade; dies reicht von der leichten Besteigung des Mont-aux-Sources vom Plateau aus bis zur jährlichen Mont-aux-Sources Challenge, wenn Querfeldeinläufer zusammenkommen, um die 50 Kilometer lange Strecke in weniger als fünf Stunden zu absolvieren.
(Wikipedia)
Wodehouse Peak Trail
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 paleontology finds have been made in the park, including dinosaur eggs and skeletons.
"Golden Gate" refers to the sandstone cliffs found on either side of the valley at the Golden Gate dam. In 1875, a farmer called J.N.R. van Reenen and his wife stopped here as they travelled to their new farm in Vuurland. He named the location "Golden Gate" when he saw the last rays of the setting sun fall on the cliffs.
In 1963, 47.92 km2 (11,840 acres) were proclaimed as a national park, specifically to preserve the scenic beauty of the area. In 1981, the park was enlarged to 62.41 km2 (15,420 acres), and in 1988, it was enlarged to 116.33 km2 (28,750 acres). In 2004, the park was announced to be joining with the neighbouring QwaQwa National Park. The amalgamation of QwaQwa National Park was completed in 2007, increasing the park's area to 340 km2 (84,000 acres).
The park is 320 km (200 mi) from Johannesburg and is close to the villages of Clarens and Kestell, in the upper regions of the Little Caledon River. The park is situated in the Rooiberge of the eastern Free State, in the foothills of the Maluti Mountains. The Caledon River forms the southern boundary of the park, as well as the border between the Free State and Lesotho. The highest peak in the park (and also in the Free State) is Ribbokkop at 2,829 m (9,281 ft) above sea level.
The park is located in the eastern highveld region of South Africa, and experiences a dry, sunny climate from June to August. It has showers, hail, and thunderstorms between October and April. It has thick snowfalls in the winter. The park has a relatively high rainfall of 800 mm (31 in) per year.
The park is an area of rich highveld and montane grassland flora. It has more than 60 grass species and a large variety of bulbs and herbs. Each of these species has its own flowering time, meaning that veld flowers can be seen throughout the summer. The park also has Afromontane forests and high-altitude Austro-Afro alpine grassland, which is scarce in South Africa. The ouhout (Leucosidea sericea), an evergreen species, is the most common tree in the park. Ouhout is a favourite habitat of beetles and 117 species occur on these trees in the park. The Lombardi poplars and weeping willows in the park are introduced species, but are kept because of their cultural and historic connection with the eastern Free State. Other exotic species in the park, for example wattle and bluegum, are systematically eradicated.
Instead of reintroducing one of the "big five" into the park, the sungazer lizard and water mongoose were reintroduced. Twelve species of mice, 10 species of carnivores, and 10 antelope species have been recorded in the park. The grey rhebuck and the mountain reedbuck were present when the park was established.
The geology of the park provides very visual "textbook" examples of Southern Africa's geological history. The sandstone formations in the park form the upper part of the Karoo Supergroup. These formations were deposited during a period of aeolian deposition towards the end of the Triassic Period. At the time of deposition, the climate of the area the park covers was becoming progressively drier until arid desert conditions set in, resulting in a land of dunes and sandy desert, with occasional scattered oases. The deposition of the sandstones ended when lava flowed out over the desert 190 million years ago.
The following sequence of geological formations is visible in the park (starting from the bottom): the Molteno Formation, Elliott Formation, Clarens Formation, and Drakensberg Formation. The yellow-brown Golden Gate and Brandwag cliffs are made up of the Clarens formation. The layers in this formation are 140 to 160 m (460 to 520 ft) thick. The Drakensberg formation comprises the basaltic lava that flowed over the desert. It forms the mountain summits in the park. On Ribbokkop, it is 600 m (2,000 ft) thick. The Elliot Formation is a red mudstone where many dinosaur fossils have been found.
The oldest dinosaur embryos ever discovered were found in the park in 1978. The eggs were from the Triassic Period (220 to 195 million years ago) and had fossilised foetal skeletons of Massospondylus, a prosauropod dinosaur. More examples of these eggs have since been found in the park. Other fossils found in the park include those of advanced cynodontia (canine toothed animals), small thecodontia (animals with teeth set firmly in the jaw), and bird-like and crocodile-like dinosaurs.
Accommodation in the park is available at Glen Reenen and Brandwag Rest camps. Caravan and camp sites with all amenities are available at Glen Reenen camp. The hotel was formerly part of Brandwag camp, but since its recent refurbishment, it is managed separately by SANParks as Golden Gate Hotel. The nearest town to Golden Gate Highlands National Park is Clarens (17 km to the west), but Phuthaditjhaba is also easily reached by a good tar road, driving through the access gate to the east of the park.
This park will be included into the Maloti-Drakensberg Transfrontier Conservation Area, Peace Park.
(Wikipedia)
Der Golden-Gate-Highlands-Nationalpark (englisch Golden Gate Highlands National Park) liegt in Südafrika, im Südosten des Freistaates nahe der Grenze zu Lesotho, und zeichnet sich besonders durch seine malerischen Felslandschaften aus. Orange oder ocker gefärbte Sandsteinfelsen ragen über das bergige Grasland auf. Außerdem gibt es Felsmalereien der San.
Der nördliche Eingang zum Park liegt bei dem Künstlerdorf Clarens.
(Wikipedia)
Sunset seen from Highlands Mountain Retreat.
Sonnenuntergang vom Highlands Mountain Retreat gesehen.
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 paleontology finds have been made in the park, including dinosaur eggs and skeletons.
"Golden Gate" refers to the sandstone cliffs found on either side of the valley at the Golden Gate dam. In 1875, a farmer called J.N.R. van Reenen and his wife stopped here as they travelled to their new farm in Vuurland. He named the location "Golden Gate" when he saw the last rays of the setting sun fall on the cliffs.
In 1963, 47.92 km2 (11,840 acres) were proclaimed as a national park, specifically to preserve the scenic beauty of the area. In 1981, the park was enlarged to 62.41 km2 (15,420 acres), and in 1988, it was enlarged to 116.33 km2 (28,750 acres). In 2004, the park was announced to be joining with the neighbouring QwaQwa National Park. The amalgamation of QwaQwa National Park was completed in 2007, increasing the park's area to 340 km2 (84,000 acres).
The park is 320 km (200 mi) from Johannesburg and is close to the villages of Clarens and Kestell, in the upper regions of the Little Caledon River. The park is situated in the Rooiberge of the eastern Free State, in the foothills of the Maluti Mountains. The Caledon River forms the southern boundary of the park, as well as the border between the Free State and Lesotho. The highest peak in the park (and also in the Free State) is Ribbokkop at 2,829 m (9,281 ft) above sea level.
The park is located in the eastern highveld region of South Africa, and experiences a dry, sunny climate from June to August. It has showers, hail, and thunderstorms between October and April. It has thick snowfalls in the winter. The park has a relatively high rainfall of 800 mm (31 in) per year.
The park is an area of rich highveld and montane grassland flora. It has more than 60 grass species and a large variety of bulbs and herbs. Each of these species has its own flowering time, meaning that veld flowers can be seen throughout the summer. The park also has Afromontane forests and high-altitude Austro-Afro alpine grassland, which is scarce in South Africa. The ouhout (Leucosidea sericea), an evergreen species, is the most common tree in the park. Ouhout is a favourite habitat of beetles and 117 species occur on these trees in the park. The Lombardi poplars and weeping willows in the park are introduced species, but are kept because of their cultural and historic connection with the eastern Free State. Other exotic species in the park, for example wattle and bluegum, are systematically eradicated.
Instead of reintroducing one of the "big five" into the park, the sungazer lizard and water mongoose were reintroduced. Twelve species of mice, 10 species of carnivores, and 10 antelope species have been recorded in the park. The grey rhebuck and the mountain reedbuck were present when the park was established.
The geology of the park provides very visual "textbook" examples of Southern Africa's geological history. The sandstone formations in the park form the upper part of the Karoo Supergroup. These formations were deposited during a period of aeolian deposition towards the end of the Triassic Period. At the time of deposition, the climate of the area the park covers was becoming progressively drier until arid desert conditions set in, resulting in a land of dunes and sandy desert, with occasional scattered oases. The deposition of the sandstones ended when lava flowed out over the desert 190 million years ago.
The following sequence of geological formations is visible in the park (starting from the bottom): the Molteno Formation, Elliott Formation, Clarens Formation, and Drakensberg Formation. The yellow-brown Golden Gate and Brandwag cliffs are made up of the Clarens formation. The layers in this formation are 140 to 160 m (460 to 520 ft) thick. The Drakensberg formation comprises the basaltic lava that flowed over the desert. It forms the mountain summits in the park. On Ribbokkop, it is 600 m (2,000 ft) thick. The Elliot Formation is a red mudstone where many dinosaur fossils have been found.
The oldest dinosaur embryos ever discovered were found in the park in 1978. The eggs were from the Triassic Period (220 to 195 million years ago) and had fossilised foetal skeletons of Massospondylus, a prosauropod dinosaur. More examples of these eggs have since been found in the park. Other fossils found in the park include those of advanced cynodontia (canine toothed animals), small thecodontia (animals with teeth set firmly in the jaw), and bird-like and crocodile-like dinosaurs.
Accommodation in the park is available at Glen Reenen and Brandwag Rest camps. Caravan and camp sites with all amenities are available at Glen Reenen camp. The hotel was formerly part of Brandwag camp, but since its recent refurbishment, it is managed separately by SANParks as Golden Gate Hotel. The nearest town to Golden Gate Highlands National Park is Clarens (17 km to the west), but Phuthaditjhaba is also easily reached by a good tar road, driving through the access gate to the east of the park.
This park will be included into the Maloti-Drakensberg Transfrontier Conservation Area, Peace Park.
(Wikipedia)
Der Golden-Gate-Highlands-Nationalpark (englisch Golden Gate Highlands National Park) liegt in Südafrika, im Südosten des Freistaates nahe der Grenze zu Lesotho, und zeichnet sich besonders durch seine malerischen Felslandschaften aus. Orange oder ocker gefärbte Sandsteinfelsen ragen über das bergige Grasland auf. Außerdem gibt es Felsmalereien der San.
Der nördliche Eingang zum Park liegt bei dem Künstlerdorf Clarens.
(Wikipedia)
Hike around Plowman's Kop via the Crack and Mudslide.
In the background you can see the Amphitheatre with the Sentinel.
Wanderung über den Plowman's Kop über Crack und Mudslide.
Im Hintergrund sieht man das Amphitheater.
The uKhahlamba-Drakensberg Park is in the KwaZulu-Natal province of South Africa, covering 2,428.13 km2 (938 sq mi) of area. The park includes Royal Natal National Park, a provincial park, and covers part of the Drakensberg, the highest mountain range in Southern Africa.
The park and the adjoining Sehlabathebe National Park in the Kingdom of Lesotho are part of the Maloti-Drakensberg Park, which was first declared a World Heritage Site on 30 November 2000. It is described by UNESCO as having "exceptional natural beauty in its soaring basaltic buttresses, incisive dramatic cutbacks, and golden sandstone ramparts... the site’s diversity of habitats protects a high level of endemic and globally threatened species, especially birds and plants... [and it] also contains many caves and rock-shelters with the largest and most concentrated group of paintings in Africa south of the Sahara".
Plans to boost tourism in the area include a long-awaited cable car project by the KZN Economic Development, Tourism and Environmental Affairs Department.
The Drakensberg mountain range is characterized by a high level of endemism of both invertebrates and vertebrates.
Most of the higher South African parts of the Drakensberg mountain range have been designated as game reserves or wilderness areas. The uKhahlamba-Drakensberg Park is also in the List of Wetlands of International Importance (under the Ramsar Convention). Adjacent to the park is the Cathkin Estates Conservation and Wildlife Sanctuary, which spans 1,044 ha (10 km2) of virgin grassland and represents the largest privately owned game park in the KwaZulu-Natal Drakensberg region.
(Wikipedia)
The Royal Natal National Park is in the KwaZulu Natal province of South Africa and forms part of the uKhahlamba Drakensberg Park World Heritage Site. Notwithstanding the name, it is actually not a South African National Park managed by the SANParks, but rather a Provincial Park managed by Ezemvelo KZN Wildlife. This park is now included into the Maloti-Drakensberg Transfrontier Conservation Area Peace Park.
The main features of the park are the Drakensberg Amphitheatre, a rock wall 5 kilometres (3.1 mi) long by up to 1,200 metres (3,900 ft) high, Mont-Aux-Sources peak where the Orange and Tugela rivers have their source, and the 948-metre (3,110 ft) Tugela Falls, the world's second-highest waterfall.
(Wikipedia)
Der uKhahlamba-Drakensberg Park (isiZulu uKhahlamba = „Barriere aus Speeren“) ist ein Nationalpark in den Drakensbergen in Südafrika. Im November 2000 wurde der Park in die UNESCO-Welterbe-Liste eingetragen. Der Park wird von der Provinzbehörde Ezemvelo KZN Wildlife verwaltet.
Der Park bedeckt eine Fläche von 2428 km². Er liegt in der Provinz KwaZulu-Natal und bildet einen 180 Kilometer langen und bis zu 20 Kilometer breiten Streifen entlang der Grenze zum Königreich Lesotho. Weitere Bestandteile des uKhahlamba-Drakensberg Park sind die getrennt liegenden Gebiete Royal-Natal-Nationalpark und Spioenkop Dam Nature Reserve weiter im Norden.
Der Park verfügt über hochaufragende Bergformationen und ist mit einem gut ausgebauten Netz von Wanderpfaden durchzogen. Basaltene, senkrecht aufragende Bergpfeiler, Bastionen aus goldbraunem Sandstein sowie skulpturierte Bögen, Höhlen, Säulen und Felswannen prägen das Landschaftsbild. Die Kette der Drakensberge im uKhahlamba-Drakensberg Park umfasst mehrere über 3000 Meter hohe Gipfel wie den Mafadi, den Giant’s Castle, den Cathedral Peak, den Monk’s Cowl, den Champagne Castle und den Njesuthi. Die Berghänge sind teilweise als Naturschutzgebiete ausgewiesen, in denen sich rund 30.000 Felsmalereien in etwa 600 Höhlen finden, die von San-Menschen über einen Zeitraum von 4000 Jahren erstellt wurden. In dieser Region entspringen die meisten großen Flüsse der Provinz KwaZulu-Natal. Sie bilden tiefe Schluchten und Täler. Einzige Straßenverbindung durch den Park nach Lesotho ist die Strecke über den Sanipass.
Es gibt eine Vielfalt endemischer Pflanzenarten, darunter Zuckerbüsche. Im Frühjahr übersäen in den Niederungen Teppiche von Wildblumen den Park, darunter Watsonia-Arten.
Zu den Vogelarten gehören Kapgeier (Gyps coprotheres) und Bartgeier (Gypaetus barbatus). Zahlreiche im Park beheimatete Wirbeltiere und Wirbellose sind endemisch. Weiterhin leben im Park Buschböcke, Ducker, Elenantilopen und Paviane.
1903 beschloss die Regierung der Kolonie Natal die Errichtung eines Naturschutzgebietes in den Drakensbergen. 1905 wurde eine klare Grenzziehung des Schutzbereichs proklamiert. 1916 wurde der Royal Natal National Park eingerichtet. Ab den 1950er Jahren wurden in den Drakensbergen diverse Naturschutzgebiete ausgewiesen, so 1951 das Kamberg Nature Reserve, 1953 das Nature Reserve de Lotheni und 1967 Vergelegen. Dabei wurde der Gewässerschutz vorangetrieben. 1973 kamen die Schutzgebiete Mdedelelo und Mkomazi hinzu.
Im Juni 2001 wurde des Maloti-Drakensberg Transfrontier Conservation Area (etwa: Maloti-Drakensberge-Grenzüberschreitendes-Erhaltungsgebiet) gegründet. Dieses verbindet den ukhahlamba-Drakensberg Park mit dem Sehlabathebe-Nationalpark in Lesotho. Ihm liegt der Anspruch an einen Peace Park (Transfrontier Conservation Area/TFCA) zugrunde. Die zwölf Kilometer lange Staatsgrenze kann zu Fuß passiert werden. Seit 2013 sind beide Nationalparks zusammen als Maloti Drakensberg Transboundary World Heritage Site in der UNESCO-Welterbe-Liste verzeichnet. Der gesamte Park ist nunmehr 2493 km² groß, wobei 65 km² der Fläche auf das Terrain Lesothos entfallen.
„… exceptional natural beauty in its soaring basaltic buttresses, incisive dramatic cutbacks, and golden sandstone ramparts … the site’s diversity of habitats protects a high level of endemic and globally threatened species, especially birds and plants … [and it] also contains many caves and rock-shelters with the largest and most concentrated group of paintings in Africa south of the Sahara. – … außergewöhnliche Schönheit der Natur in seinen aufragenden Basaltpfeilern, prägnante dramatische Einschnitte, und goldene Sandstein-Wälle … Die Vielfalt der Lebensräume beschützt ein hohes Maß an endemischen und vom Aussterben bedrohten Arten, vor allem Vögel und Pflanzen … [und es] enthält viele Höhlen und Felsnischen mit der größten und dichtesten Gruppe von Gemälden in Afrika südlich der Sahara.“
– Beschreibung des Maloti-Drakensberg Transfrontier Conservation Area auf der Website der UNESCO: Begründung zur Auswahl 2013
Teile der Drakensberg-Gebirgskette sind zu Schutzzwecken mit übergeordneter Bedeutung als Totalreservate ausgewiesen, sowie für touristische Zwecke daneben als Wildreservate. Entsprechend der Ramsar-Konvention wird der uKhahlamba Drakensberg Park auch als Schutzgut der List of Ramsar wetlands of international importance geführt. Private Eigentumsrechte hält an kleineren Gebietsteilen die Cathkin Estates Conservation and Wildlife Sanctuary.
(Wikipedia)
Der Royal Natal National Park wurde 1916 in den südafrikanischen Drakensbergen in der heutigen Provinz KwaZulu-Natal gebildet. Er ist Teil des Ukhahlamba-Drakensberg Park, der zum UNESCO-Welterbe gehört. Er gehört zu den spektakulärsten Natursehenswürdigkeiten in Afrika. Beeindruckend ist das Amphitheatre, eine mehrere Kilometer lange und etwa 1000 Meter hohe Felswand zwischen Sentinel (3165 m) und Eastern Buttress (3047 m). Auf dem flachen Gipfelplateau stehen einige Berge wie der Mont-Aux-Sources (Sesotho: Phofung) (3282 m), den 1836 die französischen Missionare Thomas Arbousset und François Daumas bestiegen und nach den Quellen von drei größeren Flüssen benannten.
Einer von diesen, der Tugela, stürzt in den Tugelafällen in fünf Stufen 948 Meter in die Tiefe (andere Angaben: knapp 3000 Fuß, 540 m). In kalten Wintern friert er in den oberen Stufen und bildet eindrucksvolle Eissäulen.
Der Royal Natal National Park ist ideal geeignet für Wanderungen mit einem Netz von klassifizierten Wegen aller Schwierigkeitsgrade; dies reicht von der leichten Besteigung des Mont-aux-Sources vom Plateau aus bis zur jährlichen Mont-aux-Sources Challenge, wenn Querfeldeinläufer zusammenkommen, um die 50 Kilometer lange Strecke in weniger als fünf Stunden zu absolvieren.
(Wikipedia)
Policeman's Helmet
The uKhahlamba-Drakensberg Park is in the KwaZulu-Natal province of South Africa, covering 2,428.13 km2 (938 sq mi) of area. The park includes Royal Natal National Park, a provincial park, and covers part of the Drakensberg, the highest mountain range in Southern Africa.
The park and the adjoining Sehlabathebe National Park in the Kingdom of Lesotho are part of the Maloti-Drakensberg Park, which was first declared a World Heritage Site on 30 November 2000. It is described by UNESCO as having "exceptional natural beauty in its soaring basaltic buttresses, incisive dramatic cutbacks, and golden sandstone ramparts... the site’s diversity of habitats protects a high level of endemic and globally threatened species, especially birds and plants... [and it] also contains many caves and rock-shelters with the largest and most concentrated group of paintings in Africa south of the Sahara".
Plans to boost tourism in the area include a long-awaited cable car project by the KZN Economic Development, Tourism and Environmental Affairs Department.
The Drakensberg mountain range is characterized by a high level of endemism of both invertebrates and vertebrates.
Most of the higher South African parts of the Drakensberg mountain range have been designated as game reserves or wilderness areas. The uKhahlamba-Drakensberg Park is also in the List of Wetlands of International Importance (under the Ramsar Convention). Adjacent to the park is the Cathkin Estates Conservation and Wildlife Sanctuary, which spans 1,044 ha (10 km2) of virgin grassland and represents the largest privately owned game park in the KwaZulu-Natal Drakensberg region.
(Wikipedia)
The Royal Natal National Park is in the KwaZulu Natal province of South Africa and forms part of the uKhahlamba Drakensberg Park World Heritage Site. Notwithstanding the name, it is actually not a South African National Park managed by the SANParks, but rather a Provincial Park managed by Ezemvelo KZN Wildlife. This park is now included into the Maloti-Drakensberg Transfrontier Conservation Area Peace Park.
The main features of the park are the Drakensberg Amphitheatre, a rock wall 5 kilometres (3.1 mi) long by up to 1,200 metres (3,900 ft) high, Mont-Aux-Sources peak where the Orange and Tugela rivers have their source, and the 948-metre (3,110 ft) Tugela Falls, the world's second-highest waterfall.
(Wikipedia)
Der uKhahlamba-Drakensberg Park (isiZulu uKhahlamba = „Barriere aus Speeren“) ist ein Nationalpark in den Drakensbergen in Südafrika. Im November 2000 wurde der Park in die UNESCO-Welterbe-Liste eingetragen. Der Park wird von der Provinzbehörde Ezemvelo KZN Wildlife verwaltet.
Der Park bedeckt eine Fläche von 2428 km². Er liegt in der Provinz KwaZulu-Natal und bildet einen 180 Kilometer langen und bis zu 20 Kilometer breiten Streifen entlang der Grenze zum Königreich Lesotho. Weitere Bestandteile des uKhahlamba-Drakensberg Park sind die getrennt liegenden Gebiete Royal-Natal-Nationalpark und Spioenkop Dam Nature Reserve weiter im Norden.
Der Park verfügt über hochaufragende Bergformationen und ist mit einem gut ausgebauten Netz von Wanderpfaden durchzogen. Basaltene, senkrecht aufragende Bergpfeiler, Bastionen aus goldbraunem Sandstein sowie skulpturierte Bögen, Höhlen, Säulen und Felswannen prägen das Landschaftsbild. Die Kette der Drakensberge im uKhahlamba-Drakensberg Park umfasst mehrere über 3000 Meter hohe Gipfel wie den Mafadi, den Giant’s Castle, den Cathedral Peak, den Monk’s Cowl, den Champagne Castle und den Njesuthi. Die Berghänge sind teilweise als Naturschutzgebiete ausgewiesen, in denen sich rund 30.000 Felsmalereien in etwa 600 Höhlen finden, die von San-Menschen über einen Zeitraum von 4000 Jahren erstellt wurden. In dieser Region entspringen die meisten großen Flüsse der Provinz KwaZulu-Natal. Sie bilden tiefe Schluchten und Täler. Einzige Straßenverbindung durch den Park nach Lesotho ist die Strecke über den Sanipass.
Es gibt eine Vielfalt endemischer Pflanzenarten, darunter Zuckerbüsche. Im Frühjahr übersäen in den Niederungen Teppiche von Wildblumen den Park, darunter Watsonia-Arten.
Zu den Vogelarten gehören Kapgeier (Gyps coprotheres) und Bartgeier (Gypaetus barbatus). Zahlreiche im Park beheimatete Wirbeltiere und Wirbellose sind endemisch. Weiterhin leben im Park Buschböcke, Ducker, Elenantilopen und Paviane.
1903 beschloss die Regierung der Kolonie Natal die Errichtung eines Naturschutzgebietes in den Drakensbergen. 1905 wurde eine klare Grenzziehung des Schutzbereichs proklamiert. 1916 wurde der Royal Natal National Park eingerichtet. Ab den 1950er Jahren wurden in den Drakensbergen diverse Naturschutzgebiete ausgewiesen, so 1951 das Kamberg Nature Reserve, 1953 das Nature Reserve de Lotheni und 1967 Vergelegen. Dabei wurde der Gewässerschutz vorangetrieben. 1973 kamen die Schutzgebiete Mdedelelo und Mkomazi hinzu.
Im Juni 2001 wurde des Maloti-Drakensberg Transfrontier Conservation Area (etwa: Maloti-Drakensberge-Grenzüberschreitendes-Erhaltungsgebiet) gegründet. Dieses verbindet den ukhahlamba-Drakensberg Park mit dem Sehlabathebe-Nationalpark in Lesotho. Ihm liegt der Anspruch an einen Peace Park (Transfrontier Conservation Area/TFCA) zugrunde. Die zwölf Kilometer lange Staatsgrenze kann zu Fuß passiert werden. Seit 2013 sind beide Nationalparks zusammen als Maloti Drakensberg Transboundary World Heritage Site in der UNESCO-Welterbe-Liste verzeichnet. Der gesamte Park ist nunmehr 2493 km² groß, wobei 65 km² der Fläche auf das Terrain Lesothos entfallen.
„… exceptional natural beauty in its soaring basaltic buttresses, incisive dramatic cutbacks, and golden sandstone ramparts … the site’s diversity of habitats protects a high level of endemic and globally threatened species, especially birds and plants … [and it] also contains many caves and rock-shelters with the largest and most concentrated group of paintings in Africa south of the Sahara. – … außergewöhnliche Schönheit der Natur in seinen aufragenden Basaltpfeilern, prägnante dramatische Einschnitte, und goldene Sandstein-Wälle … Die Vielfalt der Lebensräume beschützt ein hohes Maß an endemischen und vom Aussterben bedrohten Arten, vor allem Vögel und Pflanzen … [und es] enthält viele Höhlen und Felsnischen mit der größten und dichtesten Gruppe von Gemälden in Afrika südlich der Sahara.“
– Beschreibung des Maloti-Drakensberg Transfrontier Conservation Area auf der Website der UNESCO: Begründung zur Auswahl 2013
Teile der Drakensberg-Gebirgskette sind zu Schutzzwecken mit übergeordneter Bedeutung als Totalreservate ausgewiesen, sowie für touristische Zwecke daneben als Wildreservate. Entsprechend der Ramsar-Konvention wird der uKhahlamba Drakensberg Park auch als Schutzgut der List of Ramsar wetlands of international importance geführt. Private Eigentumsrechte hält an kleineren Gebietsteilen die Cathkin Estates Conservation and Wildlife Sanctuary.
(Wikipedia)
Der Royal Natal National Park wurde 1916 in den südafrikanischen Drakensbergen in der heutigen Provinz KwaZulu-Natal gebildet. Er ist Teil des Ukhahlamba-Drakensberg Park, der zum UNESCO-Welterbe gehört. Er gehört zu den spektakulärsten Natursehenswürdigkeiten in Afrika. Beeindruckend ist das Amphitheatre, eine mehrere Kilometer lange und etwa 1000 Meter hohe Felswand zwischen Sentinel (3165 m) und Eastern Buttress (3047 m). Auf dem flachen Gipfelplateau stehen einige Berge wie der Mont-Aux-Sources (Sesotho: Phofung) (3282 m), den 1836 die französischen Missionare Thomas Arbousset und François Daumas bestiegen und nach den Quellen von drei größeren Flüssen benannten.
Einer von diesen, der Tugela, stürzt in den Tugelafällen in fünf Stufen 948 Meter in die Tiefe (andere Angaben: knapp 3000 Fuß, 540 m). In kalten Wintern friert er in den oberen Stufen und bildet eindrucksvolle Eissäulen.
Der Royal Natal National Park ist ideal geeignet für Wanderungen mit einem Netz von klassifizierten Wegen aller Schwierigkeitsgrade; dies reicht von der leichten Besteigung des Mont-aux-Sources vom Plateau aus bis zur jährlichen Mont-aux-Sources Challenge, wenn Querfeldeinläufer zusammenkommen, um die 50 Kilometer lange Strecke in weniger als fünf Stunden zu absolvieren.
(Wikipedia)
Eine schöne Sicht von Berlin gibt's nicht nur vom Fernsehturm aus: Der Weg zum und auf den Drachenberg in Charlottenburg-Wilmersdorf lohnt sich so gut wie immer! Die komplette Skyline ist von hier aus recht gut zu erkennen, sowie die ehemalige Abhörstation auf dem Teufelsberg, genau nebenan! Ich hoffe es gefällt euch :)
©Patrick Lemoine
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Wodehouse Peak Trail
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 paleontology finds have been made in the park, including dinosaur eggs and skeletons.
"Golden Gate" refers to the sandstone cliffs found on either side of the valley at the Golden Gate dam. In 1875, a farmer called J.N.R. van Reenen and his wife stopped here as they travelled to their new farm in Vuurland. He named the location "Golden Gate" when he saw the last rays of the setting sun fall on the cliffs.
In 1963, 47.92 km2 (11,840 acres) were proclaimed as a national park, specifically to preserve the scenic beauty of the area. In 1981, the park was enlarged to 62.41 km2 (15,420 acres), and in 1988, it was enlarged to 116.33 km2 (28,750 acres). In 2004, the park was announced to be joining with the neighbouring QwaQwa National Park. The amalgamation of QwaQwa National Park was completed in 2007, increasing the park's area to 340 km2 (84,000 acres).
The park is 320 km (200 mi) from Johannesburg and is close to the villages of Clarens and Kestell, in the upper regions of the Little Caledon River. The park is situated in the Rooiberge of the eastern Free State, in the foothills of the Maluti Mountains. The Caledon River forms the southern boundary of the park, as well as the border between the Free State and Lesotho. The highest peak in the park (and also in the Free State) is Ribbokkop at 2,829 m (9,281 ft) above sea level.
The park is located in the eastern highveld region of South Africa, and experiences a dry, sunny climate from June to August. It has showers, hail, and thunderstorms between October and April. It has thick snowfalls in the winter. The park has a relatively high rainfall of 800 mm (31 in) per year.
The park is an area of rich highveld and montane grassland flora. It has more than 60 grass species and a large variety of bulbs and herbs. Each of these species has its own flowering time, meaning that veld flowers can be seen throughout the summer. The park also has Afromontane forests and high-altitude Austro-Afro alpine grassland, which is scarce in South Africa. The ouhout (Leucosidea sericea), an evergreen species, is the most common tree in the park. Ouhout is a favourite habitat of beetles and 117 species occur on these trees in the park. The Lombardi poplars and weeping willows in the park are introduced species, but are kept because of their cultural and historic connection with the eastern Free State. Other exotic species in the park, for example wattle and bluegum, are systematically eradicated.
Instead of reintroducing one of the "big five" into the park, the sungazer lizard and water mongoose were reintroduced. Twelve species of mice, 10 species of carnivores, and 10 antelope species have been recorded in the park. The grey rhebuck and the mountain reedbuck were present when the park was established.
The geology of the park provides very visual "textbook" examples of Southern Africa's geological history. The sandstone formations in the park form the upper part of the Karoo Supergroup. These formations were deposited during a period of aeolian deposition towards the end of the Triassic Period. At the time of deposition, the climate of the area the park covers was becoming progressively drier until arid desert conditions set in, resulting in a land of dunes and sandy desert, with occasional scattered oases. The deposition of the sandstones ended when lava flowed out over the desert 190 million years ago.
The following sequence of geological formations is visible in the park (starting from the bottom): the Molteno Formation, Elliott Formation, Clarens Formation, and Drakensberg Formation. The yellow-brown Golden Gate and Brandwag cliffs are made up of the Clarens formation. The layers in this formation are 140 to 160 m (460 to 520 ft) thick. The Drakensberg formation comprises the basaltic lava that flowed over the desert. It forms the mountain summits in the park. On Ribbokkop, it is 600 m (2,000 ft) thick. The Elliot Formation is a red mudstone where many dinosaur fossils have been found.
The oldest dinosaur embryos ever discovered were found in the park in 1978. The eggs were from the Triassic Period (220 to 195 million years ago) and had fossilised foetal skeletons of Massospondylus, a prosauropod dinosaur. More examples of these eggs have since been found in the park. Other fossils found in the park include those of advanced cynodontia (canine toothed animals), small thecodontia (animals with teeth set firmly in the jaw), and bird-like and crocodile-like dinosaurs.
Accommodation in the park is available at Glen Reenen and Brandwag Rest camps. Caravan and camp sites with all amenities are available at Glen Reenen camp. The hotel was formerly part of Brandwag camp, but since its recent refurbishment, it is managed separately by SANParks as Golden Gate Hotel. The nearest town to Golden Gate Highlands National Park is Clarens (17 km to the west), but Phuthaditjhaba is also easily reached by a good tar road, driving through the access gate to the east of the park.
This park will be included into the Maloti-Drakensberg Transfrontier Conservation Area, Peace Park.
(Wikipedia)
Der Golden-Gate-Highlands-Nationalpark (englisch Golden Gate Highlands National Park) liegt in Südafrika, im Südosten des Freistaates nahe der Grenze zu Lesotho, und zeichnet sich besonders durch seine malerischen Felslandschaften aus. Orange oder ocker gefärbte Sandsteinfelsen ragen über das bergige Grasland auf. Außerdem gibt es Felsmalereien der San.
Der nördliche Eingang zum Park liegt bei dem Künstlerdorf Clarens.
(Wikipedia)
Wodehouse Peak Trail
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 paleontology finds have been made in the park, including dinosaur eggs and skeletons.
"Golden Gate" refers to the sandstone cliffs found on either side of the valley at the Golden Gate dam. In 1875, a farmer called J.N.R. van Reenen and his wife stopped here as they travelled to their new farm in Vuurland. He named the location "Golden Gate" when he saw the last rays of the setting sun fall on the cliffs.
In 1963, 47.92 km2 (11,840 acres) were proclaimed as a national park, specifically to preserve the scenic beauty of the area. In 1981, the park was enlarged to 62.41 km2 (15,420 acres), and in 1988, it was enlarged to 116.33 km2 (28,750 acres). In 2004, the park was announced to be joining with the neighbouring QwaQwa National Park. The amalgamation of QwaQwa National Park was completed in 2007, increasing the park's area to 340 km2 (84,000 acres).
The park is 320 km (200 mi) from Johannesburg and is close to the villages of Clarens and Kestell, in the upper regions of the Little Caledon River. The park is situated in the Rooiberge of the eastern Free State, in the foothills of the Maluti Mountains. The Caledon River forms the southern boundary of the park, as well as the border between the Free State and Lesotho. The highest peak in the park (and also in the Free State) is Ribbokkop at 2,829 m (9,281 ft) above sea level.
The park is located in the eastern highveld region of South Africa, and experiences a dry, sunny climate from June to August. It has showers, hail, and thunderstorms between October and April. It has thick snowfalls in the winter. The park has a relatively high rainfall of 800 mm (31 in) per year.
The park is an area of rich highveld and montane grassland flora. It has more than 60 grass species and a large variety of bulbs and herbs. Each of these species has its own flowering time, meaning that veld flowers can be seen throughout the summer. The park also has Afromontane forests and high-altitude Austro-Afro alpine grassland, which is scarce in South Africa. The ouhout (Leucosidea sericea), an evergreen species, is the most common tree in the park. Ouhout is a favourite habitat of beetles and 117 species occur on these trees in the park. The Lombardi poplars and weeping willows in the park are introduced species, but are kept because of their cultural and historic connection with the eastern Free State. Other exotic species in the park, for example wattle and bluegum, are systematically eradicated.
Instead of reintroducing one of the "big five" into the park, the sungazer lizard and water mongoose were reintroduced. Twelve species of mice, 10 species of carnivores, and 10 antelope species have been recorded in the park. The grey rhebuck and the mountain reedbuck were present when the park was established.
The geology of the park provides very visual "textbook" examples of Southern Africa's geological history. The sandstone formations in the park form the upper part of the Karoo Supergroup. These formations were deposited during a period of aeolian deposition towards the end of the Triassic Period. At the time of deposition, the climate of the area the park covers was becoming progressively drier until arid desert conditions set in, resulting in a land of dunes and sandy desert, with occasional scattered oases. The deposition of the sandstones ended when lava flowed out over the desert 190 million years ago.
The following sequence of geological formations is visible in the park (starting from the bottom): the Molteno Formation, Elliott Formation, Clarens Formation, and Drakensberg Formation. The yellow-brown Golden Gate and Brandwag cliffs are made up of the Clarens formation. The layers in this formation are 140 to 160 m (460 to 520 ft) thick. The Drakensberg formation comprises the basaltic lava that flowed over the desert. It forms the mountain summits in the park. On Ribbokkop, it is 600 m (2,000 ft) thick. The Elliot Formation is a red mudstone where many dinosaur fossils have been found.
The oldest dinosaur embryos ever discovered were found in the park in 1978. The eggs were from the Triassic Period (220 to 195 million years ago) and had fossilised foetal skeletons of Massospondylus, a prosauropod dinosaur. More examples of these eggs have since been found in the park. Other fossils found in the park include those of advanced cynodontia (canine toothed animals), small thecodontia (animals with teeth set firmly in the jaw), and bird-like and crocodile-like dinosaurs.
Accommodation in the park is available at Glen Reenen and Brandwag Rest camps. Caravan and camp sites with all amenities are available at Glen Reenen camp. The hotel was formerly part of Brandwag camp, but since its recent refurbishment, it is managed separately by SANParks as Golden Gate Hotel. The nearest town to Golden Gate Highlands National Park is Clarens (17 km to the west), but Phuthaditjhaba is also easily reached by a good tar road, driving through the access gate to the east of the park.
This park will be included into the Maloti-Drakensberg Transfrontier Conservation Area, Peace Park.
(Wikipedia)
Der Golden-Gate-Highlands-Nationalpark (englisch Golden Gate Highlands National Park) liegt in Südafrika, im Südosten des Freistaates nahe der Grenze zu Lesotho, und zeichnet sich besonders durch seine malerischen Felslandschaften aus. Orange oder ocker gefärbte Sandsteinfelsen ragen über das bergige Grasland auf. Außerdem gibt es Felsmalereien der San.
Der nördliche Eingang zum Park liegt bei dem Künstlerdorf Clarens.
(Wikipedia)