The Okavango Delta in Botswana is a vast inland delta formed where the Okavango River reaches a tectonic trough at an altitude of 930–1,000 m in the central part of the endorheic basin of the Kalahari.

It is a UNESCO World Heritage Site as one of the few interior delta systems that do not flow into a sea or ocean, with a wetland system that is largely intact. All the water reaching the delta is ultimately evaporated and transpired. Each year, about 11 cubic kilometers (2.6 cu mi) of water spreads over the 6,000–15,000 km2 (2,300–5,800 sq mi) area. Some flood waters drain into Lake Ngami. The area was once part of Lake Makgadikgadi, an ancient lake that had mostly dried up by the early Holocene.

The Moremi Game Reserve is on the eastern side of the delta. The delta was named one of the Seven Natural Wonders of Africa, which were officially declared on 11 February 2013 in ArushaTanzania. On 22 June 2014, the Okavango Delta became the 1000th site to be officially inscribed on the UNESCO World Heritage List.

Okavango Delta Geography

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 (750 mi) in around one month. The waters then spread over the 250 by 150 km (155 by 93 mi) area of the delta over the next four months (March–June).

The high temperature of the delta causes rapid transpiration and evaporation, resulting in three cycles of rising and falling water levels[9] that were 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 (7 ft) variation in height across its 15,000 km2 (5,800 sq mi),[10] while the water drops about 60 m from Mohembo to Maun.[3][11][12]

 

Lagoons

Shinde Lagoon, seen from the air

When the water levels gradually recede, water remains in major canals and river beds, in waterholes and in a number of larger lagoons, which then attract increasing numbers of animals. Photo-safari camps and lodges are found near some of these lagoons. Among the larger lagoons are:

 

Salt islands

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.[13]

Chief’s Island

Chief’s Island (19°12′S 22°48′E), the largest island in the delta, was formed by a fault line which uplifted an area over 70 km long (43 mi) and 15 km wide (9.3 mi). Historically, it was reserved as an exclusive hunting area for the chief, but is now a protected area for wildlife. It now provides the core area for much of the resident wildlife when the waters rise.[14]

Climate

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 (18 in) (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 (104 °F), warm nights, and humidity levels fluctuating between 50 and 80%. From March to May, the temperature reduces, with a maximum of 30 °C (86 °F) during the day and mild to cool nights. The rains quickly dry up leading into the dry, cool winter months of June to August. Daytime temperatures at this time of year are mild to warm, but the temperature falls considerably after sunset. Nights can be cold in the delta, with temperatures barely above freezing.[15]

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 (104 °F) and the dryness is only occasionally broken by a sudden cloudburst.[16]

Fauna of the delta

A cheetah silhouetted against a sunset in the delta

The Okavango Delta is both a permanent and seasonal home to a wide variety of wildlife which is now a popular tourist attraction.[17] All of the big five game animals—the lionleopardAfrican buffaloAfrican bush elephant and rhinoceros (both black and white rhinoceros)—are present.[18]

Other species include giraffeblue wildebeestplains zebrahippopotamus,[19] impalacommon elandgreater kudusable anteloperoan antelopepukulechwewaterbucksitatungatsessebecheetah,[20] African wild dogspotted hyenablack-backed jackalcaracalservalaardvarkaardwolfbat-eared foxAfrican savanna harehoney badgercrested porcupinecommon warthogchacma baboonvervet monkey and Nile crocodile.[21]

The delta also hosts over 400 bird species, including the helmeted guineafowlAfrican fish eaglePel’s fishing owlEgyptian gooseSouth African shelduckAfrican jacanaAfrican skimmermarabou storkcrested craneAfrican spoonbillAfrican dartersouthern ground hornbillwattled crane,[22] lilac-breasted rollersecretary bird, and common ostrich.[23] Prime bird-watching areas are those with a mix of habitats such as the panhandle, the seasonal delta and the parts of the Moremi Game Reserve that are close to the water.[24]

Since 2005, the protected area has been considered a Lion Conservation Unit together with Hwange National Park.[25]

Both white and black rhino has been reintroduced by Botswana Rhino Reintroduction Project. In 1992, black rhino was estimated extinct while white rhino was left just 19 individuals.[26] From 2020 to 2021 92 rhinos were killed by poachers, prompting the Botswana government to move out all rhinos from Okavango Delta.[27] In 2019, 400 individuals of rhinos estimated left in the Botswana,[28] Of that, population left in delta region has only 40 individuals.[26]

Small gathering of lechwe antelopes, Okavango Delta

The most abundant large mammal is the lechwe, with estimates suggesting approximately 88,000 individuals.[29] The lechwe a bit larger than an impala, with elongated hooves and a water-repellent substance on its legs that enable rapid movement through knee-deep water. Lechwe graze on aquatic plants and, like the waterbuck, take to water when threatened by predators. Only the males have horns.[30]

Fish

The Okavango Delta is home to 71 fish species, including the tigerfish, species of tilapia, and various species of catfish. Fish sizes range from the 1.4 m (4.6 ft) African sharptooth catfish to the 3.2 cm (1.3 in) sickle barb. The same species are found in the Zambezi River, indicating an historic link between the two river systems.[31]

Flora of the delta

The Okavango Delta is home to 1068 plants which belong to 134 families and 530 genera.[32] There are five important plant communities in the perennial swamp: Papyrus cyperus in the deeper watersMiscanthus in the shallowly flooded sites, and Phragmites australisTypha capensis and Pycreus in between. The swamp-dominant species, which are usually found in the perennial swamp, also extend far into the seasonally inundated area.[16] Papyrus cyperus reeds beds grow best in slow flowing waters of medium depth and are prominent at the channel sides. On the islands and mainlands edges above the flooded grasslands different communities of flora are found. These species are located according to their water preference: for instance Philenoptera violacea requires little water, is found at the highest elevations in the perennial swamps, and is common on drier seasonal swamp islands. Trees restricted to islands within the perennial swamp are a mixture of the palm Hyphaene petersiana and acacias.[32][33]

The mainland in the delta is characterized by mosaic of grassland and woodland communities composed of trees, shrubs and understory herbs, basically the vegetation is notably drier than the swamp. Vachellia (acacias), BosciaCombretum and Terminalia are some of the principal genera which make up the majority of plants within the Okavango Delta. The natural phenomenon of the annual flood in the dry season and the distinct rainy season in time of low rain is the result of the exceptionally high plant diversity within the delta.[32]

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. The river’s load In the delta consists almost entirely of sand, because the clean waters of the Okavango contain little mud. 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 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.[34]

People

Hambukushu guide poles his makoro on delta floodwaters

The 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 in Angola and in the 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[35] have inhabited the area around Seronga as well as the southern delta around Maun, and a few Wayeyi[36] 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 were settled in the area around Etsha in the western Panhandle.

 

EMBARKING ON A NAMIBIAN PRIVATE TOUR PROMISES AN ENRICHING JOURNEY THROUGH THE HEART AND SOUL OF THIS ICONIC LANDMARK.

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