Botswana is a landlocked country located in Southern Africa, north of South Africa. Botswana occupies an area of 581,730 square kilometres (224,610 sq mi), of which 566,730 km2 (218,820 sq mi) are land. Botswana has land boundaries of combined length 4,347.15 kilometres (2,701.19 mi), of which the constituent boundaries are shared with Namibia, for 1,544 km (959 mi); South Africa 1,969 km (1,223 mi); Zimbabwe, 834 km (518 mi) and Zambia, 0.15 km (0.093 mi). Much of the population of Botswana is concentrated in the eastern part of the country.
The Kalahari Desert is a large semi-arid sandy savanna in Southern Africa extending for 900,000 square kilometres (350,000 sq mi), covering much of Botswana, and parts of Namibia and South Africa.
Lake Makgadikgadi was a paleolake that existed in what is now the Kalahari Desert in Botswana from 2,000,000 years BP to 10,000 years BP. It may have once covered an area of from 80,000 to 275,000 km2 and was 30 m deep. The Okavango, Upper Zambezi, and Cuando rivers once all emptied into the lake. Its remains are seen in the Makgadikgadi salt pans, one of the largest salt pans in the world.
The Cuando River is a river in south-central Africa flowing through Angola and Namibia's Caprivi Strip and into the Linyanti Swamp on the northern border of Botswana. Below the swamp, the river is called the Linyanti River and, farther east, the Chobe River, before it flows into the Zambezi River.
The Sangoan is the name given by archaeologists to a Palaeolithic tool manufacturing style which may have developed from the earlier Acheulian types. In addition to the Acheulian stone tools, bone and antler picks were also used. Sangoan toolkits were used especially for grubbing.
The Boteti River is a natural watercourse in Botswana. It derives flow from the core Okavango Delta through the Thamalakane River in Maun.
The Makgadikgadi Pan, a salt pan situated in the middle of the dry savanna of north-eastern Botswana, is one of the largest salt flats in the world. The pan is all that remains of the formerly enormous Lake Makgadikgadi, which once covered an area larger than Switzerland, but dried up tens of thousands of years ago. Recent studies of human mitochondrial DNA suggest that modern Homo sapiens first began to evolve in this region some 200,000 years ago, when it was a vast, exceptionally fertile area of lakes, rivers, marshes, woodlands and grasslands especially favorable for habitation by evolving hominins and other mammals.
The Tsodilo Hills are a UNESCO World Heritage Site (WHS), consisting of rock art, rock shelters, depressions, and caves in southern Africa. It gained its WHS listing in 2001 because of its unique religious and spiritual significance to local peoples, as well as its unique record of human settlement over many millennia. UNESCO estimates there are over 4500 rock paintings at the site. The site consists of a few main hills known as the Child Hill, Female Hill, and Male Hill.
The Kalahari Basin, also known as the Kalahari Depression, Okavango Basin or the Makgadikgadi basin, is an endorheic basin and large lowland area covering approximately 725,293 km2 covering most of Botswana and Namibia, as well as parts of Angola, South Africa, Zambia, and Zimbabwe. The outstanding physical feature in the basin, and occupying the centre, is the large Kalahari Desert.
Maun Airport is an international airport serving the town of Maun in the North-West District of Botswana. It is on the north side of the town and is accessible by shuttle bus or taxi.
Mosetse is a village in Central District of Botswana. It is located along the road from Francistown to Nata. The population was 1,661 in 2001 census. Mosetse lies along the Mosetse River, which ultimately discharges to the Sua Pan, a part of the Makgadikgadi Pan.
Mopipi is a village in Central District of Botswana. It is located close to Makgadikgadi Pan. The population was 3,066 in 2001 census. This village was named after a tree called Mopipi, which is commonly found in the region. This area has witnessed steady acidification and desertification since the Pleistocene, but perhaps most dramatically since the 19th century. In particular, the Boteti River used to flow year around in this area on its way to discharge to the Makgadikgadi Pans, but presently this flow is only in the rainy season.
Branchinella spinosa is a species within the family Thamnocephalidae. This fairy shrimp species occurs in parts of Southern Africa, notably the Makgadikgadi Pans of Botswana. Other crustacean species found in this region of Botswana in co-existence with B. spinosa include Moina belli.
The Ntwetwe Pan is a large salt pan within the Makgadikgadi region of Botswana. The Ntwetwe is one of three large pans within the Makgadikgadi, the other two being Nxai Pan and Sua Pan. Ntwetwe Pan is now a seasonal lake with filling occurring in the rainy season. Ntwetwe was first described to the European world by David Livingstone, pursuant to his explorations in this region. Significant archaeological recoveries have occurred within the Nwetwe Pan, including Stone Age tools from people who lived in this area, in an earlier time of prehistory when a large year round lake occupied the Nwetwe Pan area within the Makgadikgadi.
Branchinella ornata is a species within the family Thamnocephalidae. This fairy shrimp species is found in parts of Southern Africa, notably the Sua and Nwetwe Pans of the Makgadikgadi Pans in Botswana.
The Sua Pan or Sowa Pan is a large natural topographic depression within the Makgadikgadi region of Botswana. It is located near the village of Sowa, whose name means salt in the language of the San. The Sua salt pan is one of three large pans within the Makgadikgadi, the other two being Nxai Pan and Nwetwe Pan.
Nxai Pan is a large salt pan topographic depression which is part of the larger Makgadikgadi Pans in northeastern Botswana. It lies on the old Pandamatenga Trail, which until the 1960s was used for overland cattle drives. The area is speckled with umbrella acacias and is said to resemble the Serengeti in Tanzania. The Nxai Pan was added to the National Park System to augment the Makgadikgadi Pans National Park, thus providing an enlarged contiguous area of natural protection.
The Lepashe River is a natural watercourse in Botswana. It shares its name with the village of Lepashe, through which the river flows. The Lepashe River discharges to the Sua Pan. There are significant gravel resources along some reaches of the Lepashe River.
The Nata Bird Sanctuary, the only protected reserve in the northeastern periphery of Sowa Pan in Botswana, is a community-managed project, with assistance from the Nata Conservation Committee and national and international organizations. Founded in 1988, it opened for operations in 1993; it encompasses an area of 230 square kilometres (89 sq mi), with the objective of conservation of wildlife. The community project is managed by a Trust titled the "Kalahari Conservation Society", which has members drawn from the four villages of Nata, Sepako, Maposa and Manxotae in the vicinity of the sanctuary.
Lekhubu Island is a rock outcrop in Botswana. It is located in the Southern campus of the large natural topographic depression within the Makgadikgadi region of Botswana called the Sua Pan, which is the largest pan in Botswana. It is a two billion year old granite rock island, crescent shaped and is about one kilometre long, its slopes are littered with fossil beaches of rounded pebbles, an indication of the prehistoric lake's former water levels. Lukhubu is referred to as an island because it is surrounded by a sea of white salt.
