Etosha National Park
|Etosha National Park|
Animals at the Nebrownii waterhole
|Area||22,270 square kilometres (8,600 sq mi)|
|Established||March 22, 1907|
|Visitors||200000 (in 2010)|
|Governing body||Ministry of Environment and Tourism, Namibia|
Etosha National Park is a national park in northwestern Namibia. The park was proclaimed a game reserve on March 22, 1907 in Ordinance 88 by the Governor of German South West Africa, Dr. Friedrich von Lindequist. It was designated as Wildschutzgebiet Nr. 2 which means Game Reserve Number 2, in numerical order after West Caprivi (Game Reserve No. 1) and preceding Namib Game Reserve (No. 3). In 1958, Game Reserve No. 2 became Etosha Game Park and was elevated to status of National Park in 1967 by an act of parliament of the Republic of South Africa which administered South-West Africa during that time.
Etosha National Park spans an area of 22,270 square kilometres (8,600 sq mi) and gets its name from the large Etosha pan which is almost entirely within the park. The Etosha pan (4,760 square kilometres (1,840 sq mi)) covers 23% of the area of the total area of the Etosha National Park. The park is home to hundreds of species of mammals, birds and reptiles, including several threatened and endangered species such as the black rhinoceros.
- 1 History
- 2 Geography
- 3 Vegetation types
- 4 Fauna
- 5 Tourism
- 6 References
- 7 External links
Discovery by Europeans
Explorers Charles John Andersson and Francis Galton were the first Europeans to record the existence of the Etosha pan on 29 May 1851. The explorers were traveling with Ovambo copper ore traders when they arrived at Omutjamatunda (now known as Namutoni). The Etosha pan was discovered when they traveled north upon leaving Namutoni.
Origins of Name
The name Etosha (spelled Etotha in early literature) comes from Oshindonga word meaning Great White Place referring to the Etosha pan. The Hai//om called the pan Khubus which means "totally bare, white place with lots of dust". The pan is also known as Chums which refers to the noise made by a person's feet when walking on the clay of the pan.
Areas north of the Etosha pan were inhabited by Ovambo people, while various Otjiherero-speaking groups lived immediately outside the current park boundaries. The areas inside the park close to the Etosha pan had Khoisan-speaking Hai//om people.
When the Etosha pan was first discovered, the Hai//om people recognized the Ovambo chief at Ondonga but the Hereros did not. The Hai||om were forcibly removed from the park in the 1954, ending their hunter-gatherer lifestyle to become landless farm laborers. The Hai||om have had a recognized Traditional Authority since 2004 which helps facilitate communications between the community and the government. The government of Namibia acknowledges the park to be the home of Hai||om people and has plans to resettle displaced families on farms adjacent to the national park. Since 2007 the Government has acquired six farms directly south of the Gobaub depression in Etosha National Park. A number of families have settled on these farms under the leadership of Chief David Khamuxab, Paramount Chief of the Hai||om.
In 1885, entrepreneur William Worthington Jordan bought a huge tract of land from Ovambo chief Kambonde. The land spanned nearly 170 kilometres (110 mi) from Okaukuejo in the west to Fischer's Pan in the east. The price for the land was £300 sterling, paid for by 25 firearms, one salted horse and a cask of brandy. Dorstland Trekkers first traveled through the park between 1876 and 1879 on their way to Angola. The trekkers returned in 1885 and settled on 2,500-hectare (6,200-acre) farms given to them at no charge by Jordan. The trekkers named the area Upingtonia after the Prime Minister of the Cape Colony. The settlement had to be abandoned in 1886 after clashes with the Hai||om and defeat by Chief Nehale Mpingana.
German South-West Africa
The German Reich ordered troops to occupy the Okaukuejo, Namutoni and Sesfontein in 1886 in order to kill migrating wildlife to stop spread of rinderpest to cattle. A fort was built by the German cavalry in 1889 at the site of the Namutoni spring. On 28 January 1904, 500 men under Nehale Mpingana attacked Imperial Germany 's Schutztruppe at Fort Namutoni and completely destroyed it, driving out the colonial forces and taking over their horses and cattle. The fort was rebuilt and troops stationed once again when the area was declared a game reserve in 1907; Lieutenant Adolf Fischer of Fort Namutoni then became its first "game warden".
The present-day Etosha National Park has had many major and minor boundary changes since its inception in 1907. The major boundary changes since 1907 were because of Ordinance 18 of 1958 and Ordinance 21 of 1970.
When the Etosha area was proclaimed as Game Reserve 2 by Ordinance 88 of 1907, the park stretched from the mouths of the Kunene river and Hoarusib river on the Skeleton Coast to Namutoni in the east. The original area was estimated to be 99,526 square kilometres (38,427 sq mi), an estimate that has been corrected to about 80,000 square kilometres (31,000 sq mi). Ordinance 18 of 1958 changed the western park boundaries to exclude the area between the Kunene river and the Hoarusib river and instead include the area between Hoanib river and Uchab river, thus reducing the park's area to 55,000 square kilometres (21,000 sq mi). The Odendaal Commission's (1963) decision resulted in the demarcation of the present-day park boundary in 1970.
Etosha Ecological Institute
The Etosha Ecological Institute (EEI) was formally opened on 1 April 1974 by Adolf Brinkmann of the South-West African Administration. The institute is responsible for all management-related research in the park. Classification of vegetation, population and ecological studies on wildebeest, elephants and lions, and studies on anthrax were among the first major topics to be investigated. The EEI has collaborations with researchers from universities in Namibia, United States, United Kingdom, Germany, South Africa, Australia, Norway and Israel.
The salt pans are the most noticeable geological features in the Etosha national park. The main depression covers an area of about 5,000 square kilometres (1,900 sq mi), and is roughly 130 km (81 mi) long and as wide as 50 km (31 mi) places. The hypersaline conditions of the pan limit the species that can permanently inhabit the pan itself; occurrences of extremophile micro-organisms are present, which species can tolerate the hypersaline conditions. The salt pan is usually dry, but fills with water briefly in the summer, when it attracts pelicans and flamingos in particular.
In the dry season, winds blowing across the salt pan pick up saline dust and carry it across the country and out over the southern Atlantic. This salt enrichment provides minerals to the soil downwind of the pan on which some wildlife depends, though the salinity also creates challenges to farming.
The Etosha Pan was one of several sites throughout southern Africa in the Southern African Regional Science Initiative (SAFARI 2000). Using satellites, aircraft, and ground-based data from sites such as Etosha, partners in this program collected a wide variety of data on aerosols, land cover, and other characteristics of the land and atmosphere to study and understand the interactions between people and the natural environment.
The dolomite hills on the southern border of the park near the Andersson entrance gate are called Ondundozonananandana, meaning place where young boy herding cattle went to never return, probably implying a high density of predators like leopards in the hills, giving the mountains its English name of Leopard Hills. The Halali area is also home to dolomite hills within the park, with one hill inside the camp and the nearby Twee Koppies. Western Etosha is also dominated by dolomite hills which is the only place in the park that has mountain zebra.
The national park of Etosha has a desert climate of savanna. The annual average temperature is 25°C. In winter, the temperatures are of neighborhood 5°C and in summer, they can border 45°C. There is a big daily thermal amplitude and saisonière.
The precipitation are of neighborhood 266 mm /year. He can arrive that it does not rain during 1 complete year. But, when the rain arises during thunderstorms, she(it) is intense is regongle the dried up rivers, allowing animals and plants to have access to the water so rare in this part(party) of West Africa. The regularity of the precipitation is uncertain, it is raining to rain in summer the time(weather) of a thunderstorm, or that it does not rain for months. Fires can arise in summer because of the drought and the high temperatures of the Namibian air.
|Climate data for Etosha, Kunene, Namibie (1981–2010 averages)|
|Record high °C (°F)||30.5
|Average high °C (°F)||22.6
|Daily mean °C (°F)||12.3
|Average low °C (°F)||5.6
|Record low °C (°F)||−6.6
|Average precipitation mm (inches)||50.2
|Average relative humidity (%)||67||50||43||38||25||18||12||12||24||34||45||53||35|
The pans in the park are mostly devoid of vegetation with the exception of the halophytic Sporobolus salsus, a protein-rich grass that is used by grazers such as blue wildebeest and springbok. The areas around the Etosha pan also have other halophytic vegetation including grasses such as Sporobolus spicatus and Odyssea paucinervis and shrubs such as Suaeda articulata.
Most of the park is savanna woodlands except for areas close to the pan. Mopane is the most common tree, estimated to be around 80% of all trees in the park. The sandveld of north-eastern corner of Etosha is dominated by acacia and Terminalia trees. Tamboti trees characterize the woodlands south of the sandveld.
Other types of vegetation
Dwarf shrub savanna occurs areas close to the pan and is home to several small shrubs including a halophytic succulent Salsola etoshensis. Thorn bush savanna occurs close to the pan on limestone and alkaline soils and is dominated by acacia species such as Acacia nebrownii, Acacia luederitzii, Acacia melliferra, Acacia hebeclada and Acacia tortilis.
Grasslands in the park are mainly around the Etosha pan where the soil is sandy. Depending on the soil and the effects of the pan, grasslands could be dominated by one of the Eragrostis, Sporobolus, Monelytrum, Odyssea or Enneapogon species.
By 1881, large game mammals like elephants, rhinoceroses and lions had been nearly exterminated in the region. The proclamation of the game reserve helped some of the animals recover, but some species like buffalo and wild dogs have been extinct since the middle of the 20th century.
Prof. P. Schoemann, a writer from Otjiwarango, was appointed game warden in 1951 and he considered the grasslands to be severely overgrazed. A bone meal plant was constructed near Rietfontein and culling of zebras and wildebeests began in 1952. Official records indicate 293 zebras and 122 wildebeest were processed at the plant, but conservationists claimed thousands had been culled and successfully forced the plant's closure during the same year.
The drought that began in the year 1980 resulted in the largest capture and culling operation in the history of the park. 2235 mountain zebras and 450 plains zebras were captured, culled or sold. 525 elephants were culled and processed at a temporary abattoir near Olifantsrus.
Commonly seen mammals in the park, past and present, are listed in the table below
|African bush elephant||common||Etosha's elephants belong to the group of elephants in northwestern Namibia and southern Angola. They are the tallest elephants in Africa, but mineral deficiencies mean that they have very short tusks.|
|Southern white rhinoceros||rare||Reintroduced recently after a long absence|
|South-western black rhinoceros||not disclosed publicly||Odendaal Commission's plan in 1963 severely reduced the habitat of the rhinoceros as most of their preferred habitat fell outside the park. Relocation programs have existed since then to increase the population of rhinos within the protected boundaries of the park.|
|African buffalo||extinct||The last known record of buffalo in the park is from an observation of a young bull killed by lions on the Andoni plains in the 1950s.|
|Angolan giraffe G. c. angolensis||common||A 2009 genetic study on this subspecies suggests that the northern Namib Desert and Etosha National Park populations form a separate subspecies.|
|Southwest African lion||common|
|South African cheetah||uncommon|
|Black-footed cat||very rare|
|Black-backed jackal||very common|
|Cape wild dog||extinct|
|African ground squirrel||very common|
|Ground pangolin (Manis temminckii)||uncommon|
|Plains zebra||very common|
|Mountain zebra||locally common||Seen only in western Etosha|
This overview is only one indication of the diversity of birds in the park and is not a complete list.
All lodging and camping accommodation inside the park is managed by Namibia Wildlife Resorts (NWR). There five sites inside the park with lodges and three of the sites have facilities for camping. All sites have game-proof fences.
Okaukuejo was founded as a German South-West Africa military outpost in 1897 in an effort to control spread of foot-and-mouth disease. It later served as a police station and it was formally opened as a rest camp in 1955. The Okaukuejo tower was built in 1963 modeled after the old police station tower in the area. Okaukuejo has a restaurant, a post office, souvenir shops, two swimming pools and a tourist information center where visitors can record their daily observations. There is an observation deck at the Okaukuejo waterhole, which is floodlit at night for the benefit of tourists staying overnight, to observe nocturnal wildlife at the waterhole.
Namutoni is also a former police and military station in the eastern part of the park, 123 kilometres (76 mi) from Okaukuejo. Fort Namutoni was rebuilt in 1957 when it served as a rest camp for winter visitors to the park.
The Halali rest camp was opened in 1967 and is located about midway between Okaukuejo and Namutoni.
Onkoshi is an exclusive property inside the park and is located near Stinkwater
Tourists are not allowed to go west of Ozonjuitji m'bari and the only exception to that rule are registered Namibian tour operators and guests staying at Dolomite Camp. It was built in 2010 and can be accessed from the Galton gate or through the park along the 19S latitude road (19e Breëdtegaard).
- Historical Review of the Etosha Region and its subsequent administration as a National Park, H.H. Berry; Madoqua 1997, 20(1): 3-12
- Lindeque, M. and Archibald, T.J. 1991. Seasonal wetlands in Owambo and the Etosha National Park. Madoqua 17(2): 129-133
- Trümpelmann, G.P.J. 1948. Die Boer in Suid-wes Afrika.
- Born in Etosha. Ute Dieckmann (2009)
- "Namibia Heroes and Heroines". Namibia 1-on-1. Retrieved 28 January 2012.
- C. Michael Hogan. 2010
- Trees and shrubs of the Etosha National Park and in northern and central Namibia; Cornelia Berry and Blythe Loutit
- Etosha Fact Sheet 2
- A Review of Fauna and Flora Associated with Coastal and Inland Saline Flats from Namibia with Special Reference to the Etosha Pan. Peter L. Cunningham and Willem Jankowitz
- Etosha Ecological Institute, Okaukuejo.
- Etosha Park Profile
- On the clover trail. Eugène Joubert. 1996
- Brenneman, R. A.; Louis, E. E. Jr; Fennessy, J. (2009). "Genetic structure of two populations of the Namibian giraffe, Giraffa camelopardalis angolensis". African Journal of Ecology 47 (4): 720–28. doi:10.1111/j.1365-2028.2009.01078.x.
- Etosha National Park: Guidebook to the Waterholes and Animals. Timothy Osborne, Wilferd Versveld, Paul van Schalkwyk. 2003
- "Etosha National Park, Namibia". NASA Earth Observatory.
- C.Michael Hogan. 2010. Extremophile. eds. E.Monosson and C.Cleveland. Encyclopedia of Earth. National Council for Science and the Environment, Washington DC.
|Wikimedia Commons has media related to Etosha National Park.|
- Namibia Park Brochures
- Ministry of Environment and Tourism page
- Etosha on PBS
- Etosha Travel Guide
- Etosha Travel Information