Namib-Naukluft National Park

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Namib-Naukluft Park, Namibia
Namib-Naukluft Sand Dunes (2011).jpg
Sand dunes near Sossusvlei
Namibia protected areas.svg
Red pog.svg
Location Namibia
Nearest city Windhoek
Coordinates 24°32′47″S15°19′47″E / 24.54639°S 15.32972°E / -24.54639; 15.32972
Area49,768 km2 (19,216 sq mi)
Established1907
Governing bodyMinistry of Environment and Tourism

The Namib-Naukluft Park is a national park in western Namibia, situated between the coast of the Atlantic Ocean and the edge of the Great Escarpment. It encompasses part of the Namib Desert (considered the world's oldest desert), the Naukluft mountain range, and the lagoon at Sandwich Harbour. The best-known area of the park and one of the main visitor attractions in Namibia is Sossusvlei, a clay pan surrounded by dunes, and Sesriem, a small canyon of the Tsauchab. The desert research station of Gobabeb is situated within the park.

Contents

Location and description

With an overall area of 49,768 km2 (19,216 sq mi), the Namib-Naukluft National Park was at the time of its last expansion the largest game park in Africa and the fourth largest in the world. [1] It consists of a strip of land on the Atlantic Ocean, including 1,609 kilometres (1,000 mi) of sea, that extends roughly 600 kilometres (370 mi) north-to-south from the Swakop River to the B4 road to Lüderitz. [2]

Wildlife

Ancient dunes near Sossusvlei, in the relatively frequently visited center of the national park, accessible by road from Sesriem. NamibNaukluftParkDunes.JPG
Ancient dunes near Sossusvlei, in the relatively frequently visited center of the national park, accessible by road from Sesriem.

A surprising collection of creatures survives in the hyper-arid region, including snakes, geckos, unusual insects, hyenas, gemsboks, springboks, leopards, African wildcats, cape foxes, baboons, caracals, bat-eared foxes and jackals.

Geography

The region is characterised by high, isolated inselbergs and kopjes (the Afrikaans term for rocky outcrops), made up of dramatic blood-red granites, rich in feldspars and sandstone. The easternmost part of the park covers the Naukluft Mountains.

More moisture comes in as a fog off the Atlantic Ocean than falls as rain, with the average of 106 millimeters of rainfall per year concentrated in February and April.

The winds that bring in the fog are also responsible for creating the park's towering sand dunes, whose burnt orange color is a sign of their age. The orange color develops over time as iron in the sand is oxidized, like rusty metal; the older the dune, the brighter the color.

These dunes are the tallest in the world, in places rising more than 300 meters (almost 1000 feet) above the desert floor. The dunes taper off near the coast, and lagoons, wetlands, and mudflats located along the shore attract hundreds of thousands of birds.

'Namib' means "open space", and the Namib Desert gave its name to form Namibia – "land of open spaces".

History

The park was established in 1907 when the German Colonial Administration proclaimed three game reserves in German South West Africa. Today's Namib-Naukluft park was proclaimed as "Game Reserve No. 3". The other two were the Omuramba Omatako and Etosha. The northern border of the reserve was five kilometres (three miles) south of the Swakop River, and the southern border was ten kilometres (six miles) south of the Kuiseb River, so that the park included the Kuiseb but excluded the Swakop due to the economic activities at its banks. After World War I the South African administration of South West Africa confirmed the proclamation of the Germans. For the Namib-Naukluft Park, the area of Sandwich Harbour was added in 1941, and a small extension of the southern border followed in 1962. [3]

In 1966 "Game Reserve No. 3" was deproclaimed, and the Namib Desert Park was established in its stead. The Namib Desert Park included a small area north of the Swakop River where Welwitschia grow, as well as the Moon Landscape east of Swakopmund. In 1979 two more large areas were added. The Naukluft Mountain Zebra Park was included so that the Naukluft Mountains now formed part of the protected area. It previously comprised 14 commercial farms that were bought by the government to protect the Hartmann mountain zebra. The second area added was a 1,600-kilometre (1,000 mi) strip of the Atlantic Ocean, making the Namib-Naukluft Park Namibia's first marine reserve. [3]

The park's present boundaries were established in 1986 when the government was given control over parts of the Sperrgebiet , an area restricted for diamond mining. This vast strip of land has remained inaccessible to the general population but is now part of the Namib-Naukluft Park. [3]

See also

Related Research Articles

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At 824,292 km2 (318,261 sq mi), Namibia is the world's thirty-fourth largest country. After Mongolia, Namibia is the second least densely populated country in the world. Namibia got its name from the Namib desert that stretches along the coast of the Atlantic. It is also known for its wildlife.

<span class="mw-page-title-main">Namib</span> Desert in Southern Africa

The Namib is a coastal desert in Southern Africa. According to the broadest definition, the Namib stretches for more than 2,000 kilometres (1,200 mi) along the Atlantic coasts of Angola, Namibia, and northwest South Africa, extending southward from the Carunjamba River in Angola, through Namibia and to the Olifants River in Western Cape, South Africa. The Namib's northernmost portion, which extends 450 kilometres (280 mi) from the Angola-Namibia border, is known as Moçâmedes Desert, while its southern portion approaches the neighboring Kalahari Desert. From the Atlantic coast eastward, the Namib gradually ascends in elevation, reaching up to 200 kilometres (120 mi) inland to the foot of the Great Escarpment. Annual precipitation ranges from 2 millimetres (0.079 in) in the aridest regions to 200 millimetres (7.9 in) at the escarpment, making the Namib the only true desert in southern Africa. Having endured arid or semi-arid conditions for roughly 55–80 million years, the Namib may be the oldest desert in the world and contains some of the world's driest regions, with only western South America's Atacama Desert to challenge it for age and aridity benchmarks.

<span class="mw-page-title-main">Kuiseb River</span> River in Erongo, Namibia

The Kuiseb River is an ephemeral river in western-central Namibia. Its source is in the Khomas Highland west of Windhoek. From there it flows westwards through the Namib-Naukluft National Park and the Namib desert to Walvis Bay. Several settlements of the Topnaar people are on the banks of the lower Kuiseb, for instance Homeb, Sandfontein, Rooibank, and Utuseb. Inflows of the Kuiseb are Gomab, Ojab, Chausib, Gaub, Koam, Nausgomab and Goagos.

<span class="mw-page-title-main">Skeleton Coast</span> Atlantic coast of northern Namibia and southern Angola

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Swakopmund is a city on the coast of western Namibia, 352 km (219 mi) west of the Namibian capital Windhoek via the B2 main road. It is the capital of the Erongo administrative district. As of 2011, the town had 44,725 inhabitants and 196 km2 (76 sq mi) of land.

<span class="mw-page-title-main">Kaokoveld</span> Desert ecoregion in Angola and Namibia

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<span class="mw-page-title-main">Sossusvlei</span> Salt and clay pan in the Namib Desert,  Namibia

Sossusvlei is a salt and clay pan surrounded by high red dunes, located in the southern part of the Namib Desert, in the Namib-Naukluft National Park of Namibia. The name "Sossusvlei" is often used in an extended meaning to refer to the surrounding area. These landmarks are some of the major visitor attractions of Namibia.

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<span class="mw-page-title-main">Swakop River</span> River in Namibia

The Swakop River is a major river in western central Namibia. Its source is in the Khomas Highland. From there it flows westwards through the town of Okahandja, the historic mission station at Gross Barmen, and the settlement of Otjimbingwe. It then crosses the Namib desert and reaches the Atlantic Ocean at Swakopmund. The Swakop is an ephemeral river; its run-off is roughly 40 million cubic metres per annum.

<span class="mw-page-title-main">Tsauchab</span> River in central Namibia

The Tsauchab is an ephemeral river in the Hardap Region of central Namibia. Its source is in the southern Naukluft Mountains, from where it flows westwards through the Namib-Naukluft National Park into Sossusvlei, an endorheic basin. The lower river has in the past had a slightly different courses and also formed two other basins, the Deadvlei and the Hiddenvlei.

<span class="mw-page-title-main">Gobabeb</span> Research station in the Namib Desert

The Gobabeb Namib Research Institute, short: Gobabeb, is a centre for dry land training and research in Namibia. It is located in the Namib Desert, 120 kilometres (75 mi) south-east of Walvis Bay.

<span class="mw-page-title-main">Tourism in Namibia</span> Economic sector in Namibia

Tourism in Namibia is a major industry, contributing N$7.2 billion to the country's gross domestic product. Annually, over one million travelers visit Namibia, with roughly one in three coming from South Africa, then Germany and finally the United Kingdom, Italy and France. The country is among the prime destinations in Africa and is known for ecotourism which features Namibia's extensive wildlife.

<span class="mw-page-title-main">B4 road (Namibia)</span> National highway of Namibia

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<span class="mw-page-title-main">Namib Desert Horse</span> Breed of horse

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Acanthoproctus diadematus is an armoured katydid, bush-cricket, or ground cricket endemic to the Namib Desert of southern Africa, where it lives in the tall sand dunes along the Kuiseb River in Namib-Naukluft National Park. The katydid feeds on the !nara melon endemic to the area.

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<span class="mw-page-title-main">Dorob National Park</span> National park of Namibia

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<span class="mw-page-title-main">Husab Mine</span>

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References

  1. Namib Naukluft Park
  2. "Namib-Naukluft National Park | Namibia". Wild Safari Guide. Retrieved 2021-02-04.
  3. 1 2 3 Bridgeford, Peter (2008). "One Hundred Years of Conservation. From Game Reserve No.3 to Namib-Naukluft Park" (PDF). Journal. Namibia Scientific Society. 56 (56): 45–62.