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The Okavango Delta
Okavango Delta
(or Okavango Grassland) (formerly spelled "Okovango" or "Okovanggo") in Botswana
Botswana
is a very large, swampy inland delta formed where the Okavango River
Okavango River
reaches a tectonic trough in the central part of the endorheic basin of the Kalahari. All the water reaching the delta is ultimately evaporated and transpired, and does not flow into any sea or ocean. Each year, about 11 cubic kilometers of water spread over the 6,000- to 15,000-km2 area. Some flood waters drain into Lake Ngami.[1] The Moremi Game Reserve, a National Park, is on the eastern side of the Delta. The scale and magnificence of the Okavango Delta
Okavango Delta
helped it secure a position as one of the Seven Natural Wonders of Africa, which were officially declared on February 11, 2013, in Arusha, Tanzania.[2] On 22 June 2014, the Okavango Delta became the 1000th site to be officially inscribed on the UNESCO
UNESCO
World Heritage List.[3][4] The area was once part of Lake Makgadikgadi, an ancient lake that mostly dried up by the early Holocene. Although the Okavango Delta
Okavango Delta
is widely believed to be the world's largest inland delta, it is not. Africa
Africa
alone has two larger similar geological features: the Sudd
Sudd
on the Nile
Nile
in South Sudan, and the Inner Niger Delta
Inner Niger Delta
in Mali.[5]

Contents

1 Geography

1.1 Floods 1.2 Water flow 1.3 Salt islands 1.4 Chief’s Island

2 Climate 3 Wildlife

3.1 Fish 3.2 Lechwe 3.3 Plants 3.4 Game lodges

4 People 5 Molapo's 6 Possible threats 7 Gallery 8 See also 9 References 10 Sources 11 External links

Geography[edit] Floods[edit] The Okavango is produced by seasonal flooding. The Okavango River drains the summer (January–February) rainfall from the Angola highlands and the surge flows 1,200 km in around one month. The waters then spread over the 250- by 150-km area of the delta over the next four months (March–June). The high temperature of the delta causes rapid transpiration and evaporation, resulting in a cycle of rising and falling water level that was not fully understood until the early 20th century. The flood peaks between June and August, during Botswana’s dry winter months, when the delta swells to three times its permanent size, attracting animals from kilometres around and creating one of Africa’s greatest concentrations of wildlife. The delta is very flat, with less than 2 m variation in height across its 15,000 km2.[6] Water flow[edit] Every year, about 11 km3 (11,000,000,000,000 l) of water flow into the delta. Roughly 60% is consumed through transpiration by plants, 36% by evaporation, 2% percolates into the aquifer system; and 2% flows into Lake Ngami. This turgid outflow means that the delta is unable to flush out the minerals carried by the river and is liable to become increasingly salty and uninhabitable. Water salinity is reduced by salt collecting around plant roots as most of the incoming water is transpired by plants. Peat fires might contribute to deposit salt into layers below the surface. The low salinity of the water also means that the floods do not greatly enrich the floodplain with nutrients.[citation needed] Salt islands[edit] The agglomeration of salt around plant roots leads to barren white patches in the centre of many of the thousands of islands, which have become too salty to support plants, aside from the odd salt-resistant palm tree. Trees and grasses grow in the sand around the edges of the islands that have not become too salty yet. About 70% of the islands began as termite mounds (often Macrotermes spp.), where a tree then takes root on the mound of soil.[citation needed] Chief’s Island[edit] Chief’s Island, the largest island in the delta, was formed by a fault line which uplifted an area over 70 km long and 15 km wide. Historically, it was reserved as an exclusive hunting area for the chief. It now provides the core area for much of the resident wildlife when the waters rise.[citation needed] Climate[edit]

Aerial view of delta as floodwaters recede, August 2012

The Delta's profuse greenery is not the result of a wet climate; rather, it is an oasis in an arid country. The average annual rainfall is 450 mm (approximately one third that of its Angolan catchment area) and most of it falls between December and March in the form of heavy afternoon thunderstorms. December to February are hot wet months with daytime temperatures as high as 40°C, warm nights, and humidity levels fluctuating between 50 and 80%. From March to May, the temperature becomes far more comfortable with a maximum of 30°C during the day and mild to cool nights. The rains quickly dry up leading into the dry, cold winter months of June to August. Daytime temperatures at this time of year are mild to warm, but the temperature begins to fall after sunset. Nights can be surprisingly cold in the delta, with temperatures barely above freezing.[citation needed] The September to November span has the heat and atmospheric pressure build up once more, as the dry season slides into the rainy season. October is the most challenging month for visitors - daytime temperatures often push past 40°C and the dryness is only occasionally broken by a sudden cloudburst.[citation needed] Wildlife[edit]

A South African cheetah
South African cheetah
is silhouetted against a sunset in Okavango Delta.

The Okavango delta is both a permanent and seasonal home to a wide variety of wildlife which is now a popular tourist attraction.[7] Species include African bush elephant, African buffalo, hippopotamus, lechwe, tsessebe, sitatunga, blue wildebeest, South African giraffe, Nile
Nile
crocodile, Southwest African lion, South African cheetah, African leopard, brown hyena, spotted hyena, springbok, greater kudu, sable antelope, impala, south-central black rhinoceros, southern white rhinoceros, Burchell's zebra, common warthog, chacma baboon, and vervet monkey. Notably, the endangered Cape wild dog
Cape wild dog
survives within the Okavango Delta,[8] exhibiting one of the richest pack densities in Africa. The delta also includes over 400 species of birds, including African fish eagle, Pel's fishing owl, crested crane, lilac-breasted roller, hammerkop, South African ostrich, and sacred ibis. The majority of the estimated 200,000 large mammals in and around the delta are not year-round residents. They leave with the summer rains to find renewed fields of grass to graze and trees to browse, then make their way back as winter approaches. Large herds of buffalo and elephant total about 30,000 beasts.[citation needed] Fish[edit] The Okavango Delta
Okavango Delta
is home to 71 fish species, including tigerfish, tilapia, and various species of catfish. Fish sizes range from 1.4 m African sharptooth catfish
African sharptooth catfish
to 3.2 cm sickle barb. The same species are found in the Zambezi River, indicating a historic link between the two river systems.[9] Lechwe[edit]

Small gathering of lechwe antelopes, Okavango Delta

The most populous large mammal is the lechwe antelope, with more than 60,000. It is a bit larger than an impala with elongated hooves and a water-repellent substance on their legs that enables rapid movement through knee-deep water. They graze on aquatic plants, and like the waterbuck, take to water when threatened by predators. Only the males have horns. Plants[edit] Papyrus and reed rafts make up a large part of the Okavango's vegetation. During the flood season, they float well above the sandy river bed with roots dangling free in the water. This gap between bed and roots is used as shelter by crocodiles. The plants of the delta play an important role in providing cohesion for the sand. The banks or levees of a river normally have a high mud content, and this combines with the sand in the river’s load to continuously build up the river banks. In the delta, because the clean waters of the Okavango contain almost no mud, the river’s load consists almost entirely of sand. The plants capture the sand, acting as the glue and making up for the lack of mud and in the process creating further islands on which more plants can take root. This process is not important in the formation of linear islands. They are long and thin and often curved like a gently meandering river, because they are actually the natural banks of old river channels which over time have become blocked up by plant growth and sand deposition, resulting in the river changing course and the old river levees becoming islands. Due to the flatness of the Delta, and the large tonnage of sand flowing into it from the Okavango River, the floor of the delta is slowly but constantly rising. Where channels are today, islands will be tomorrow and then new channels may wash away these existing islands.[10] Game lodges[edit]

Tented Lodge in the Okavango-Delta

The Botswana
Botswana
Okavango Game Lodges (2011) cater to small numbers of guests, each one operating in its own private concession area. Many lodges have low environmental-effect policies.[11] People[edit]

Hambukushu guide poles his makoro on delta floodwaters

The Okavango Delta
Okavango Delta
peoples consist of five ethnic groups, each with its own ethnic identity and language. They are Hambukushu (also known as Mbukushu, Bukushu, Bukusu, Mabukuschu, Ghuva, Haghuva), Dceriku (Dxeriku, Diriku, Gciriku, Gceriku, Giriku, Niriku), Wayeyi (Bayei, Bayeyi, Yei), Bugakhwe (Kxoe, Khwe, Kwengo, Barakwena, G/anda) and anikhwe (Gxanekwe, //tanekwe, River Bushmen, Swamp Bushmen, G//ani, //ani, Xanekwe). The Hambukushu, Dceriku, and Wayeyi have traditionally engaged in mixed economies of millet/sorghum agriculture, fishing, hunting, the collection of wild plant foods, and pastoralism. The Bugakhwe and anikwhe are Bushmen, who have traditionally practised fishing, hunting, and the collection of wild plant foods; Bugakhwe used both forest and riverine resources, while the anikhwe mostly focused on riverine resources. The Hambukushu, Dceriku, and Bugakhwe are present along the Okavango River
Okavango River
in Angola
Angola
and in the Caprivi Strip
Caprivi Strip
of Namibia, and small numbers of Hambukushu and Bugakhwe are in Zambia, as well. Within the Okavango Delta, over the past 150 years or so, Hambukushu, Dceriku, and Bugakhwe have inhabited the Panhandle and the Magwegqana in the northeastern Delta. anikhwe have inhabited the Panhandle and the area along the Boro River through the Delta, as well as the area along the Boteti River. The Wayeyi have inhabited the area around Seronga
Seronga
as well as the southern Delta around Maun, and a few Wayeyi live in their putative ancestral home in the Caprivi Strip. Within the past 20 years many people from all over the Okavango have migrated to Maun, the late 1960s and early 1970s over 4,000 Hambukushu refugees from Angola
Angola
were settled in the area around Etsha in the western Panhandle. The Okavango Delta
Okavango Delta
has been under the political control of the Batawana (a Tswana nation) since the late 18th century.[12] Led by the house of Mathiba I, the leader of a Bangwato offshoot, the Batawana established complete control over the delta in the 1850s as the regional ivory trade exploded.[13] Most Batawana, however, have traditionally lived on the edges of the delta, due to the threat that tsetse fly poses to their cattle. During a hiatus of some 40 years, the tsetse fly retreated and most Batawana lived in the swamps from 1896 through the late 1930s. Since then, the edge of the delta has become increasingly crowded with its growing human and livestock populations.

Flood-control bunds for flood recession cropping in the molapo of the Okavango, Botswana

Molapo's[edit] After the flooding season, the waters in the lower parts of the delta, near the base, recede, leaving moisture behind in the soil. This residual moisture is used for planting fodder and other crops that can thrive on it. This land is locally known as molapo. During 1974 to 1978, the floods were more intensive than normal and flood recession cropping was not possible, so severe food and fodder shortages occurred. In response, the Molapo Development Project was initiated. It protected the molapo areas with bunds to control the flooding and prevent severe flooding. The bunds are provided with sluice gates so the stored water can be released and flood recession cropping can start. [14] Possible threats[edit] The Namibian government has presented plans to build a hydropower station in the Zambezi Region, which would regulate the Okavango's flow to some extent. While proponents argue that the effect would be minimal, environmentalists argue that this project could destroy most of the rich animal and plant life in the Delta.[15] Other threats include local human encroachment and regional extraction of water in both Angola
Angola
and Namibia.[16][17] The award-winning South African filmmaker and conservationist Rick Lomba warned in the 1980s of the threat of cattle invasion to the area. His documentary The End of Eden vividly portrays this and his lobbying on behalf of the delta helped to preserve its integrity. Gallery[edit]

Okavango Delta
Okavango Delta
seen from Spot Satellite

Elephants in the Okavango Delta
Okavango Delta
seen from a mokoro (small boat)

A buffalo herd in the southern part of the Okavango Delta

The Okavango Delta
Okavango Delta
viewed from a Cessna at 1,200 ft

Water lilies in the delta

Girl gathering food in the Okavango Delta

Waiting for the hippos in the delta

Hippos as seen from a small boat in the Okavango

A pair of saddle-billed storks

Hyperolius argus
Hyperolius argus
(reed frog) in the Okavango Delta

Astronaut photograph of the delta

See also[edit]

Wetlands portal

Okavango Basin

References[edit]

^ Cecil Keen. 1997 ^ http://sevennaturalwonders.org/africa Seven Natural Wonders of Africa ^ Centre, UNESCO
UNESCO
World Heritage. "World Heritage List reaches 1000 sites with inscription of Okavango Delta
Okavango Delta
in Botswana". whc.unesco.org. Retrieved 4 April 2018.  ^ Centre, UNESCO
UNESCO
World Heritage. "Twenty six new properties added to World Heritage List at Doha meeting". whc.unesco.org. Retrieved 4 April 2018.  ^ T.S. McCarthy. 1993. The great inland deltas of Africa, Journal of African Earth Sciences, vol. 17, no. 3, pp. 275-291 ^ http://blog.africabespoke.com/okavango-delta-part-2/ Okavango Delta ^ Bradley, John H. (October 2009). "Gliding in a Mokoro
Mokoro
Through the Okavango Delta, Botswana". Cape Town to Cairo Website. CapeTowntoCairo.com. Retrieved 2009-11-10.  ^ C. Michael Hogan. 2009 ^ "Archived copy" (PDF). Archived from the original (PDF) on 6 July 2011. Retrieved 2 February 2011.  ^ " Okavango Delta
Okavango Delta
– Part 2 -". blog.africabespoke.com. Retrieved 4 April 2018.  ^ http://www.botswanaokavango.com/okavangodeltalodges.html ^ Moanaphuti Segolodi, "Ditso Tsa Batawana," 1940. https://www.academia.edu/12170767/Ditso_Tsa_Batawana_by_Moanaphuti_Segolodi_1940 ^ Barry Morton, "The Hunting Trade and the Reconstruction of Northern Tswana Societies after the Difaqane, 1838-1880," South African Historical Journal 36 (1997): 220-239. http://www.tandfonline.com/doi/abs/10.1080/02582479708671276 ^ L.F. Kortenhorst et al., 1986. Development of flood-recession cropping in the molapo's of the Okavango Delta, Botswana. Published in Annual Report 1986, p. 8 – 19 International Institute for Land Reclamation and Improvement Wageningen, The Netherlands (public domain). On line: [1] ^ "FindArticles.com - CBSi". findarticles.com. Retrieved 4 April 2018.  ^ "Threats - Okavango Delta". www.okavangodelta.com. Retrieved 4 April 2018.  ^ [2]

Sources[edit]

P. Allison. 2007. Whatever You Do, Don't Run: True Tales Of A Botswana Safari Guide J. Bock. 2002. Learning, Life History, and Productivity: Children’s lives in the Okavango Delta
Okavango Delta
of Botswana. Human Nature 13(2). 161-198. Full text C. Michael Hogan. 2009. Painted Hunting Dog: Lycaon pictus, GlobalTwitcher.com, ed. N. Stromberg Cecil Keen. 1997. Okavango Delta

External links[edit]

Wikimedia Commons has media related to Okavango Delta.

Wikivoyage has a travel guide for Okavango Delta.

Conservation International Earth-Touch.com Okavango Delta
Okavango Delta
HD Videos Flow : information for Okavango Delta
Okavango Delta
planning is the weblog of the Library of the Harry Oppenheimer Okavango Research Institute The Ngami Times is Ngamiland's weekly newspaper Official Botswana
Botswana
Government site on Moremi Game Reserve, inside the Okavango Delta Picture gallery of wildlife in the Okavango Delta Wild Entrust International Seven Natural Wonders of Africa Discovery Channel - Kalahari
Kalahari
Flood Flood-recession cropping in the molapos of the Okavango Delta Okavango Research Institute Current Okavango water levels, weather data and satellite images 1986 Documentary The End of Eden by Rick Lomba Top 25 Photographs Southern African Game Reserves - Okavango Delta

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