South Africa - Golden Gate Highlands National Park
Oribi Loop
Burchell's Zebra
Steppenzebra
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)
Burchell's zebra (Equus quagga burchellii) is a southern subspecies of the plains zebra. It is named after the British explorer and naturalist William John Burchell. Common names include the bontequagga, Damaraland zebra, and Zululand zebra (Gray, 1824). Burchell's zebra is the only subspecies of zebra which may be legally farmed for human consumption.
Like most plains zebras, females and males are relatively the same size, standing 1.1 to 1.4 meters (3.75 to 4.6 feet) at the shoulder. They weigh between 485 to 550 pounds. Year-round reproduction observed in this subspecies in Etosha National Park, Namibia, concludes synchronization of a time budget between males and females, possibly explaining the lack of sexual dimorphism.
Damara zebras are described as being striped on the head, the neck, and the flanks, and sparsely down the upper segments of the limbs then fading to white. One or two shadow stripes rest between the bold, broad stripes on the haunch. This main, distinguishing characteristic sets the Zuzuland Zebra apart from the other subspecies. Gray (1824), observed a distinct dorsal line, the tail only bristly at the end, and the body distinctly white. The dorsal line is narrow and becomes gradually broader in the hinder part, distinctly margined with white on each side.
Like most plains zebras, Burchells live in small family groups. These can be either harem or bachelor groups, with harem groups consisting of one stallion and one to six mares and their most recent foals, and bachelor groups containing two to eight unattached stallions. The males in bachelor herds are often the younger or older stallions of the population, as they are most likely not experienced enough or strong enough to defend breeding rights to a group of females from challengers. These small groups often congregate together in larger herds around water and food sources, but still maintain their identity as family units while in the population gatherings.
Formerly, the Burchell's zebra range was centered north of the Vaal/Orange river system, extending northwest via southern Botswana to Etosha and the Kaokoveld, and southeast to Swaziland and KwaZulu-Natal. Now extinct in the middle portion, it survives at the northwestern and southeastern ends of the distribution.
Burchell's zebra migrates the longest distance of any terrestrial animal in Africa, traveling 160 miles one way. They migrate from the Chobe River in Namibia to Nxai Pan National Park in Botswana. Their migration follows a straight north–south route almost entirely within the Kavango–Zambezi Transfrontier Conservation Area (KAZA).
Like other plains zebras, Burchell's zebras must have populated the African plains in impressive numbers. Associations of thousands have been reported. The wild herds were thought to have disappeared by 1910, and the last known captive individual died in the Berlin Zoo in 1918. As European settlement spread northward from the Cape to colonial southern Rhodesia, this subspecies was thought to have been hunted to extinction.
However, Groves and Bell concluded in their 2004 publication that "the extinct true Burchell's zebra" is a phantom. Careful study of the original zebra populations in Zululand and Swaziland, and of skins harvested on game farms in Zululand and Natal, has revealed that a certain small proportion shows similarity to what now is regarded as typical burchellii. The type localities of the two subspecies Equus quagga burchellii (Burchell's zebra) and Equus quagga antiquorum (Damaraland zebra) are so close to each other that they suggest that the two are in fact one, and therefore the older of the two names should take precedence over the younger. They therefore say that the correct name for the southernmost subspecies must be burchellii, not antiquorum.[9] The subspecies Equus quagga burchellii still exists in KwaZulu-Natal and in Etosha. Equus quagga burchellii can be found in a number of zoos in the United States including the following: the Cincinnati Zoo, Columbus Zoo, Naples Zoo, Nashville Zoo, Woodland Park Zoo, etc.
(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)
Das Steppenzebra (Equus quagga) oder Pferdezebra ist ein Zebra aus der Familie der Pferde (Equidae) und gehört zur Ordnung der Unpaarhufer (Perissodactyla). Es stellt heute die häufigste Zebra-Art in Afrika dar und ist vom Nordosten bis in den Süden des Kontinents verbreitet. Es lebt gesellig in kleinen Herdenverbänden und ernährt sich hauptsächlich von Gräsern. Im Gegensatz zu den anderen heutigen Pferdearten kommt es auch in teilweise geschlossenen Landschaften vor. Der Bestand, dessen größte Population heute in der Serengeti lebt, gilt als nicht gefährdet. Es werden sechs rezente Unterarten unterschieden, die sich meistens deutlich in der Streifenzeichnung voneinander abheben.
(Wikipedia)
South Africa - Golden Gate Highlands National Park
Oribi Loop
Burchell's Zebra
Steppenzebra
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)
Burchell's zebra (Equus quagga burchellii) is a southern subspecies of the plains zebra. It is named after the British explorer and naturalist William John Burchell. Common names include the bontequagga, Damaraland zebra, and Zululand zebra (Gray, 1824). Burchell's zebra is the only subspecies of zebra which may be legally farmed for human consumption.
Like most plains zebras, females and males are relatively the same size, standing 1.1 to 1.4 meters (3.75 to 4.6 feet) at the shoulder. They weigh between 485 to 550 pounds. Year-round reproduction observed in this subspecies in Etosha National Park, Namibia, concludes synchronization of a time budget between males and females, possibly explaining the lack of sexual dimorphism.
Damara zebras are described as being striped on the head, the neck, and the flanks, and sparsely down the upper segments of the limbs then fading to white. One or two shadow stripes rest between the bold, broad stripes on the haunch. This main, distinguishing characteristic sets the Zuzuland Zebra apart from the other subspecies. Gray (1824), observed a distinct dorsal line, the tail only bristly at the end, and the body distinctly white. The dorsal line is narrow and becomes gradually broader in the hinder part, distinctly margined with white on each side.
Like most plains zebras, Burchells live in small family groups. These can be either harem or bachelor groups, with harem groups consisting of one stallion and one to six mares and their most recent foals, and bachelor groups containing two to eight unattached stallions. The males in bachelor herds are often the younger or older stallions of the population, as they are most likely not experienced enough or strong enough to defend breeding rights to a group of females from challengers. These small groups often congregate together in larger herds around water and food sources, but still maintain their identity as family units while in the population gatherings.
Formerly, the Burchell's zebra range was centered north of the Vaal/Orange river system, extending northwest via southern Botswana to Etosha and the Kaokoveld, and southeast to Swaziland and KwaZulu-Natal. Now extinct in the middle portion, it survives at the northwestern and southeastern ends of the distribution.
Burchell's zebra migrates the longest distance of any terrestrial animal in Africa, traveling 160 miles one way. They migrate from the Chobe River in Namibia to Nxai Pan National Park in Botswana. Their migration follows a straight north–south route almost entirely within the Kavango–Zambezi Transfrontier Conservation Area (KAZA).
Like other plains zebras, Burchell's zebras must have populated the African plains in impressive numbers. Associations of thousands have been reported. The wild herds were thought to have disappeared by 1910, and the last known captive individual died in the Berlin Zoo in 1918. As European settlement spread northward from the Cape to colonial southern Rhodesia, this subspecies was thought to have been hunted to extinction.
However, Groves and Bell concluded in their 2004 publication that "the extinct true Burchell's zebra" is a phantom. Careful study of the original zebra populations in Zululand and Swaziland, and of skins harvested on game farms in Zululand and Natal, has revealed that a certain small proportion shows similarity to what now is regarded as typical burchellii. The type localities of the two subspecies Equus quagga burchellii (Burchell's zebra) and Equus quagga antiquorum (Damaraland zebra) are so close to each other that they suggest that the two are in fact one, and therefore the older of the two names should take precedence over the younger. They therefore say that the correct name for the southernmost subspecies must be burchellii, not antiquorum.[9] The subspecies Equus quagga burchellii still exists in KwaZulu-Natal and in Etosha. Equus quagga burchellii can be found in a number of zoos in the United States including the following: the Cincinnati Zoo, Columbus Zoo, Naples Zoo, Nashville Zoo, Woodland Park Zoo, etc.
(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)
Das Steppenzebra (Equus quagga) oder Pferdezebra ist ein Zebra aus der Familie der Pferde (Equidae) und gehört zur Ordnung der Unpaarhufer (Perissodactyla). Es stellt heute die häufigste Zebra-Art in Afrika dar und ist vom Nordosten bis in den Süden des Kontinents verbreitet. Es lebt gesellig in kleinen Herdenverbänden und ernährt sich hauptsächlich von Gräsern. Im Gegensatz zu den anderen heutigen Pferdearten kommt es auch in teilweise geschlossenen Landschaften vor. Der Bestand, dessen größte Population heute in der Serengeti lebt, gilt als nicht gefährdet. Es werden sechs rezente Unterarten unterschieden, die sich meistens deutlich in der Streifenzeichnung voneinander abheben.
(Wikipedia)