Northern Rhodesia became the Republic of Zambia on 24 October 1964, with Kaunda as the first president.
At independence, despite its considerable mineral wealth, Zambia faced major challenges. Domestically, there were few trained and educated Zambians capable of running the government, and the economy was largely dependent on foreign expertise.[citation needed] There were over 70,000 British in Zambia in 1964, who were of great economic importance.[10] During the next decade, Kaunda's regime supported movements such as UNITA in Angola; the Zimbabwe African People's Union (ZAPU); the African National Congress (ANC) in South Africa; and the South West Africa People's Organization (SWAPO).[citation needed] Kaunda developed close relations with communist regimes in theSoviet Union and the People's Republic of China. Kaunda also developed a close friendship with Iraqi dictator Saddam Hussein.[11][dubious ]
Conflict with Rhodesia resulted in the closure of the border with that country in 1973 and severe problems with international transport and power supply. However, the Kariba hydroelectric station on the Zambezi River provided sufficient capacity to satisfy the country's requirements for electricity (despite the fact that the control centre was on the Rhodesian side of the border). A railway to the Tanzanian port of Dar es Salaam, built with Chinese assistance, reduced Zambian dependence on railway lines south to South Africa and west through an increasingly troubled Angola. Until the completion of the railway, however, Zambia's major artery for imports and the critical export of copper was along the TanZam Road, running from Zambia to the port cities in Tanzania. The Tazama oil pipeline was also built from Dar-es-Salaam to Ndola in Zambia.
By the late 1970s, Mozambique and Angola had attained independence from Portugal. Zimbabwe achieved independence in 1980 in accordance with the 1979 Lancaster House Agreement. Zambia's problems, however, were not solved. Civil war in the former Portuguese colonies created an influx of refugees and caused continuing transportation problems. The Benguela railway, which extended west through Angola, was essentially closed to traffic from Zambia by the late 1970s. Zambia's strong support for the ANC (despite both the Zambian ANC and the SA ANC being banned within Zambia), which had its external headquarters in Lusaka, created security problems as South Africa raided South African ANC military training camps in Zambia.
In the mid-1970s, the price of copper, Zambia's principal export, suffered a severe decline worldwide. In Zambia's situation, the cost of transporting the copper great distances to market was an additional strain. Zambia turned to foreign and international lenders for relief, but, as copper prices remained depressed, it became increasingly difficult to service its growing debt. By the mid-1990s, despite limited debt relief, Zambia's per capita foreign debt remained among the highest in the world.
In June 1990 riots against Kaunda accelerated. Many protesters were killed by the regime in breakthrough June 1990 protests. Kaunda faced one coup attempt in 1990. In 1991, Kaunda agreed to re-institute multiparty democracy (having instated one party rule under the Chona Commission of 1972) and was replaced by multiparty elections.
In the 2000s, the economy stabilized, attaining single-digit inflation in 2006–2007, real GDP growth, decreasing interest rates, and increasing levels of trade. Much of its growth is due to foreign investment in Zambia's mining sector and higher copper prices on the world market. All this led to Zambia being courted enthusiastically by aid donors, and saw a surge, in investor confidence in the country reflected in a growing number of investors.
Main article: Politics of Zambia
Zambian politics take place in a framework of a presidential representative democratic republic, whereby the President of Zambia is both head of state and head of government in a pluriform multi-party system. The government exercises executive power, while legislative power is vested in both the government and parliament. Zambia became a republic immediately upon attaining independence in October 1964.
[edit]Subdivisions
Main article: Subdivisions of Zambia
Zambia is divided into nine provinces, each administered by an appointed deputy minister. Each province is subdivided into several districts with a grand total of 72 districts. The provinces are:
[edit]Geography
Main article: Geography of Zambia
See also: List of settlements in Zambia
Zambia is a landlocked country in southern Africa, with a tropical climate and consists mostly of high plateau, with some hills and mountains, dissected by river valleys. At 752,614 km2 (290,586 sq mi) it is the 39th-largest country in the world (after Chile) and slightly larger than the US state of Texas. The country lies mostly between latitudes 8° and 18°S, and longitudes 22° and34°E.
Zambia is drained by two major river basins: theZambezi basin in the south covering about three-quarters of the country; and the Congo basin in the north covering about one-quarter of the country. A very small area in the northeast forms part of the internal drainage basin of Lake Rukwain Tanzania.
In the Zambezi basin, there are a number of major rivers flowing wholly or partially through Zambia: the Kabompo, Lungwebungu, Kafue, Luangwa, and the Zambezi itself, which flows through the country in the west and then forms its southern border with Namibia, Botswana and Zimbabwe. Its source is in Zambia but it diverts into Angola, and a number of its tributaries rise in Angola's central highlands. The edge of the Cuando Riverfloodplain (not its main channel) forms Zambia's southwestern border, and via the Chobe River that river contributes very little water to the Zambezi because most is lost by evaporation).[12]
Two of the Zambezi's longest and largest tributaries, the Kafue and the Luangwa, flow mainly in Zambia. Their confluences with the Zambezi are on the border with Zimbabwe at Chirundu and Luangwa town respectively. Before its confluence, the Luangwa River forms part of Zambia's border with Mozambique. From Luangwa town, the Zambezi leaves Zambia and flows into Mozambique, and eventually into the Mozambique Channel.
The Zambezi falls about 100 metres (328 ft) over the 1.6 km (0.99 mi) wide Victoria Falls, located in the south-west corner of the country, subsequently flowing into Lake Kariba. The Zambezi valley, running along the southern border, is both deep and wide. From Lake Kariba going east it is formed by grabens and like the Luangwa, Mweru-Luapula, Mweru-wa-Ntipa and Lake Tanganyika valleys, is a rift valley.
The north of Zambia is very flat with broad plains. In the west the most notable being theBarotse Floodplain on the Zambezi, which floods from December to June, lagging behind the annual rainy season (typically November to April). The flood dominates the natural environment and the lives, society and culture of the inhabitants and those of other smaller, floodplains throughout the country.
In Eastern Zambia the plateau which extends between the Zambezi and Lake Tanganyika valleys is tilted upwards to the north, and so rises imperceptibly from about 900 m (2,953 ft) in the south to 1,200 m (3,937 ft) in the centre, reaching 1,800 m (5,906 ft) in the north near Mbala. These plateau areas of northern Zambia have been categorised by the World Wildlife Fund as a large section of the Central Zambezian Miombo woodlands ecoregion.
Eastern Zambia shows great diversity. The Luangwa Valley splits the plateau in a curve north east to south west, extended west into the heart of the plateau by the deep valley of the Lunsemfwa River. Hills and mountains are found by the side of some sections of the valley, notably in its north-east the Nyika Plateau (2,200 m/7,218 ft) on the Malawi border, which extend into Zambia as the Mafinga Hills, containing the country's highest point, Kongera (2,187 m/7,175 ft). The Muchinga Mountains, the watershed between the Zambezi and Congo drainage basins, run parallel to the deep valley of the Luangwa River and form a sharp backdrop to its northern edge, although they are almost everywhere below 1,700 m (5,577 ft). Their culminating peak Mumpu is at the western end and at 1,892 m (6,207 ft) is the highest point in Zambia away from the eastern border region. The border of the Congo Pedicle was drawn around this mountain.
The southernmost headstream of the Congo River rises in Zambia and flows through its north firstly as the Chambeshi and then, after theBangweulu Swamps as the Luapula, which forms part of the border with the Democratic Republic of the Congo. The Luapula flows south then west before it turns north until it enters Lake Mweru. The lake's other major tributary is the Kalungwishi River, which flows into it from the east. The Luvua River drains Lake Mweru, flowing out of the northern end to the Lualaba River (Upper Congo River).
Lake Tanganyika is the other major hydrographic feature that belongs to the Congo basin. Its south-eastern end receives water from theKalambo River, which forms part of Zambia's border with Tanzania. This river has Africa's second highest uninterrupted waterfall, the Kalambo Falls.
[edit]Climate
Main article: Climate of Zambia
The climate of Zambia is tropical modified by elevation. In the Köppen climate classification, most of the country is classified as humid subtropical or tropical wet and dry, with small stretches of semi-arid steppe climate in the south-west and along the Zambezi valley.
There are two main seasons, the rainy season (November to April) corresponding to summer, and the dry season (May/June to October/November), corresponding to winter. The dry season is subdivided into the cool dry season (May/June to August), and the hot dry season (September to October/November). The modifying influence of altitude gives the country pleasant subtropical weather rather than tropical conditions during the cool season of May to August.[13] However, average monthly temperatures remain above 20 °C (68 °F) over most of the country for eight or more months of the year.