Geography of Tanzania
Tanzania comprises many lakes, national parks, and Africa's highest point, Mount Kilimanjaro (5,895 m or 19,341 ft). Northeast Tanzania is mountainous, while the central area is part of a large plateau covered in grasslands. The country also contains the southern portion of Lake Victoria on its northern border with Uganda and Kenya.
|• Total||945,087 km2 (364,900 sq mi)|
|Coastline||1,424 km (885 mi)|
|Borders||4,161 km (2,586 mi)|
|Highest point||Mount Kilimanjaro |
5,895 metres (19,341 ft)
|Lowest point||Indian Ocean |
0 metres (0 ft)
|Longest river||Rufiji River |
600 km (370 mi)
|Largest lake||Lake Victoria 59,947 km2 (23,146 sq mi)|
|Exclusive economic zone||241,888 km2 (93,393 sq mi)|
Northeast Tanzania exhibits a mountainous terrain and includes Mount Meru, an active volcano, Mount Kilimanjaro, a dormant volcano, and the Usambara and Pare mountain ranges. Kilimanjaro attracts thousands of tourists each year. West of those mountains is the Gregory Rift, which is the eastern arm of the Great Rift Valley. On the floor of the rift are a number of large salt lakes, including Natron in the north, Manyara in the south, and Eyasi in the southwest. The rift also encompasses the Crater Highlands, which includes the Ngorongoro Conservation Area and the Ngorongoro Crater. Just to the south of Lake Natron is Ol Doinyo Lengai with an elevation of 3,188 m (10,459 ft), the world's only active volcano to produce natrocarbonatite lava. To the west of the Crater Highlands lies Serengeti National Park, which is famous for its lions, leopards, elephants, rhinoceroses, and buffalo plus the annual migration of millions of white bearded wildebeest. Just to the southeast of the park is Olduvai Gorge, where many of the oldest hominid fossils and artifacts have been found.
Further northwest is Lake Victoria on the Kenya–Uganda–Tanzania border. This is the largest lake in Africa by surface area and is traditionally named as the source of the Nile River. Southwest of this, separating Tanzania from the Democratic Republic of the Congo, is Lake Tanganyika. This lake is estimated to be the second deepest lake in the world after Lake Baikal in Siberia. The western portion of the country between Lakes Victoria, Tanganyika, and Malawi consists of flat land that has been categorised by the World Wildlife Fund as part of the Central Zambezian Miombo woodlands ecoregion. Just upstream from the Kalambo Falls, there is one of the most important archaeological sites in Africa. Tanzania's Southern Highlands are in the southwestern part of the country, around the northern end of Lake Malawi. Mbeya is the largest city in the Southern Highlands.
The centre of Tanzania is a large plateau, which is part of the East African Plateau. The southern half of this plateau is grassland within the Eastern Miombo woodlands ecoregion, the majority of which is covered by the huge Selous National Park. Further north the plateau is arable land and includes the national capital, Dodoma.
The eastern coast contains Tanzania's largest city and former capital, Dar es Salaam. Just north of this city lies the Zanzibar Archipelago, a semi-autonomous territory of Tanzania which is famous for its spices. The coast is home to areas of East African mangroves, mangrove swamps that are an important habitat for wildlife on land and in the water.
Eastern and central Tanzania are drained by rivers that empty into the Indian Ocean. The major rivers are, from north to south, the Pangani, Wami, Ruvu, Rufiji, Matandu, Mbwemkuru, and the Ruvuma River, which forms the southern border with Mozambique.
The Southern Eastern Rift area of north-central Tanzania is made up of several endorheic basins, which have no outlet to the sea and drain into salt and/or alkaline lakes. Lake Rukwa in west-central Tanzania, is another endorheic basin.
Tanzania has a tropical climate but has regional variations due to topography. In the highlands, temperatures range between 10 and 20 °C (50 and 68 °F) during cold and hot seasons respectively. The rest of the country has temperatures rarely falling lower than 20 °C (68 °F). The hottest period extends between November and February (25–31 °C or 77.0–87.8 °F) while the coldest period occurs between May and August (15–20 °C or 59–68 °F).
Seasonal rainfall is driven mainly by the migration of the Intertropical Convergence Zone. It migrates southwards through Tanzania in October to December, reaching the south of the country in January and February, and returning northwards in March, April, and May. This causes the north and east of Tanzania to experience two distinct wet periods – the short rains (or "Vuli") in October to December and the long rains (or "Masika") from March to May – while the southern, western, and central parts of the country experience one wet season that continues October through to April or May.
The onset of the long rains averages 25 March and the cessation averages 21 May. A warmer-than-normal South Atlantic Ocean coupled with a cooler-than-normal Eastern Indian Ocean often causes the onset to be delayed.
- total: 947,300 square kilometres (365,800 sq mi)
- land: 885,800 square kilometres (342,000 sq mi)
- water: 61,500 square kilometres (23,700 sq mi)
- total: 3,861 kilometres (2,399 mi)
- border countries: Burundi 451 kilometres (280 mi), Kenya 769 kilometres (478 mi), Malawi 475 kilometres (295 mi), Mozambique 756 kilometres (470 mi), Rwanda 217 kilometres (135 mi), Uganda 396 kilometres (246 mi), Zambia 338 kilometres (210 mi), Democratic Republic of the Congo 459 kilometres (285 mi)
Coastline: 1,424 kilometres (885 mi)
- exclusive economic zone: 241,888 km2 (93,393 sq mi) and 200 nmi (370.4 km; 230.2 mi)
- territorial sea: 12 nmi (22.2 km; 13.8 mi)
Terrain: plains along coast; central plateau; highlands in north, south
Irrigated land: 1,843 square kilometres (712 sq mi) (2003)
Total renewable water resources: 96.27 cubic kilometres (23.10 cu mi) (2011)
- flooding on the central plateau during the rainy season; drought
- volcanism: limited volcano activity; Ol Doinyo Lengai (elevation 2,962 metres (9,718 ft)) has emitted lava in recent years; other historically active volcanoes include Kieyo and Meru
Environment - current issues: soil degradation; deforestation; desertification; destruction of coral reef threatens marine habitats; recent droughts affected marginal agriculture; wildlife threatened by illegal hunting and trade, especially for ivory
Environment - international agreements:
- party to:
- United Nations Framework Convention on Climate Change
- Kyoto Protocol to the United Nations Framework Convention on Climate Change
- United Nations Convention to Combat Desertification in Those Countries Experiencing Serious Drought and/or Desertification, Particularly in Africa
- Convention on International Trade in Endangered Species of Wild Fauna and Flora
- Basel Convention on the Control of Transboundary Movements of Hazardous Wastes and Their Disposal
- United Nations Convention on the Law of the Sea
- Vienna Convention for the Protection of the Ozone Layer
- Convention on Wetlands of International Importance, especially as Waterfowl Habitat
Specific geographic regionsEdit
This is a list of the extreme points of Tanzania, the points that are farther north, south, east or west than any other location.
- Northernmost point - unnamed point on the border with Uganda in the Kagera river immediately east of the Ugandan town of Kikagati, Kagera Region
- Easternmost point - Mnazi, Mtwara Region
- Easternmost point (mainland) - unnamed headland immediately east of the town of Mwambo, Mtwara Region
- Southernmost point - unnamed location on the border with Mozambique in the Ruvuma River, Ruvuma Region
- Westernmost point - unnamed headland immediately west of Ujiji, Kigoma Region
- "Regions of Tanzania", Statoids, last updated 25 July 2012
- Tanzania in figures 2012, National Bureau of Statistics, Ministry of Finance, June 2013, page 9 Archived November 26, 2013, at the Wayback Machine
- "UNDP Climate Change Country Profiles: Tanzania", C. McSweeney (University of Oxford), M. New (University of Oxford and Tyndall Centre for Climate Change Research), and G. Lizcano (University of Oxford)
- "The onset and cessation of the 'long rains' in eastern Africa and their interannual variability", Theoretical and Applied Climatology, authored by P. Camberlin and R. E. Okoola, vol. 75, pages 43-54, 2003
- The World Factbook - Tanzania, U.S. Central Intelligence Agency, updated 29 April 2013