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Satellite image of Okavango Delta, with national borders added Typical region in the Okavango Delta, with free canals and lakes, swamps and islandsThe Okavango Delta [2] (or Okavango Grassland; formerly spelled "Okovango" or "Okovanggo") in Botswana is a vast inland delta formed where the Okavango River reaches a tectonic trough at an altitude of 930–1,000 metres (3,050–3,280 ft) [3] in ...
Location in Botswana. Coordinates: Country: Botswana: District: North-West District (Botswana) ... Okavango Delta region is one of the subdistricts of Ngamiland ...
The Makgadikgadi pans are clearly visible to the right of the dark-green broom-shaped Okavango Delta in this satellite image of Botswana The main water source is the Nata River , called Amanzanyama in Zimbabwe , where it rises at Sandown about 37 mi (59.5 km) from Bulawayo .
Maun Airport serves as the main gateway to the Okavango Delta and the Moremi Game Reserve. Many tour operators offer chartered flights over the Delta and to Botswana destinations such as the Makgadikgadi Pans, one of the largest seasonal wetlands in Africa. Servicing the many lodges in the area is a major activity, including the transport of ...
The Okavango continues through the Caprivi Strip of Namibia into Botswana, where it splits into a number of distributaries to form the Okavango Delta, a large inland delta that becomes a seasonally flooded grassland. After the Okavango Delta, the waters of the basin enter a zone of strong evaporation, already within the Kalahari Desert ...
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A Tented Lodge at Okavango River near Shakawe (2017) The village is served by Shakawe Airport. It is the gateway to the northern part of the Okavango Delta and the Linyanti area. Direct charter flights are operated to the aerodrome, with the main airline in the area being AirShakawe. Flight is the most efficient form of transport in the area.
The Thamalakane River is a river located in Botswana, Africa, at the southern end of the Okavango Delta.It has no well defined beginning and no clear end ().It is the result of the Thamalakane fault - which began to form about two million years ago by the geological process of rifting that is currently splitting Africa apart along the East African Rift.