NAMIBIA - GEOGRAPHY AND HISTORY

 Windhoek

Namibia, officially the Republic of Namibia (Afrikaans: Republiek van Namibië, German: About this sound Republik Namibia (help·info)), is a country in southern Africa whose western border is the Atlantic Ocean. It shares land borders with Angola and Zambia to the north, Botswana to the east and South Africa to the south and east. Although it does not border with Zimbabwe, less than 200 meters of riverbed (essentially the Zambia/Botswana border) separates them at their closest points. It gained independence from South Africa on 21 March 1990, following the Namibian War of Independence. Its capital and largest city is Windhoek. Namibia is a member state of the United Nations (UN), the Southern African Development Community (SADC), the African Union (AU), and the Commonwealth of Nations.

The dry lands of Namibia were inhabited since early times by Bushmen, Damara, and Namaqua, and since about the 14th century AD by immigrating Bantu who came with the Bantu expansion. It became a German Imperial protectorate in 1884 and remained a German colony until the end of World War I. In 1920, the League of Nations mandated the country to South Africa, which imposed its laws and, from 1948, its apartheid policy.

Uprisings and demands by African leaders led the UN to assume direct responsibility over the territory. It recognized the South West Africa People’s Organization (SWAPO) as the official representative of the Namibian people in 1973. Namibia, however, remained under South African administration during this time. Following internal violence, South Africa installed an interim administration in Namibia in 1985. Namibia obtained full independence from South Africa in 1990, with the exception of Walvis Bay and the Penguin Islands, which remained under South African control until 1994.

Namibia has a population of 2.1 million people and a stable multi-party parliamentary democracy. Agriculture, herding, tourism and the mining industry – including mining for gem diamonds, uranium, gold, silver, and base metals – form the backbone of Namibia's economy. Given the presence of the arid Namib Desert, it is one of the least densely populated countries in the world. Approximately half the population live below the international poverty line, and the nation has suffered heavily from the effects of HIV/AIDS, with 15% of the adult population infected with HIV in 2007.

History
The name of the country is derived from the Namib Desert, considered to be the oldest desert in the world. Before its independence in 1990, the area was known first as German South-West Africa (Deutsch-Südwestafrika), then as South-West Africa, reflecting the colonial occupation by the Germans and the South Africans (technically on behalf of the British crown reflecting South Africa's dominion status within the British Empire).

Pre-colonial period
The dry lands of Namibia were inhabited since early times by Bushmen, Damara, Nama, and since about the 14th century AD, by immigrating Bantu who came with the Bantu expansion from central Africa. From the late 18th century onwards, Orlam clans from the Cape Colony crossed the Orange River and moved into the area that today is southern Namibia. Their encounters with the nomadic Nama tribes were largely peaceful. The missionaries accompanying the Orlams were well received by them, the right to use waterholes and grazing was granted against an annual payment. On their way further northwards, however, the Orlams encountered clans of the Herero tribe at Windhoek, Gobabis, and Okahandja which were less accommodating. The Nama-Herero War broke out in 1880, with hostilities ebbing only when Imperial Germany deployed troops to the contested places and cemented the status quo between Nama, Orlams, and Herero.

The first Europeans to disembark and explore the region were the Portuguese navigators Diogo Cão in 1485 and Bartolomeu Dias in 1486; still the region was not claimed by the Portuguese crown. However, like most of Sub-Saharan Africa, Namibia was not extensively explored by Europeans until the 19th century, when traders and settlers arrived, principally from Germany and Sweden. In the late 19th century Dorsland trekkers crossed the area on their way from the Transvaal to Angola. Some of them settled in Namibia instead of continuing their journey, even more returned to South-West African territory after the Portuguese tried to convert them to Catholicism and forbade their language at schools.

German rule
Namibia became a German colony in 1884 to forestall British encroachment and was known as German South-West Africa (Deutsch-Südwestafrika). However, the Palgrave mission by the British governor in Cape Town had determined that only the natural deep-water harbour of Walvis Bay (Walfisch in German, Walvis in Afrikaans, Whale in English) was worth occupying – and this was annexed to the Cape province of British South Africa. From 1904 to 1907, the Herero and the Namaqua took up arms against the Germans and in the subsequent Herero and Namaqua genocide, 10,000 Nama (half the population) and approximately 65,000 Hereros (about 80% of the population) were killed. The survivors, when finally released from detention, were subjected to a policy of dispossession, deportation, forced labor, racial segregation and discrimination in a system that in many ways anticipated apartheid. Most Africans were confined to so-called native territories, which later under South African rule post-1949 were turned into "homelands" (Bantustans). Indeed, some historians have speculated that the German genocide in Namibia was a model used by Nazis in the Holocaust, but most scholars say that episode was not especially influential for the Nazis, who were children at the time. However, the father of Luftwaffe commander Hermann Göring was a one-time German colonial governor of Namibia and has a street named after him in Swakopmund. The memory of genocide remains relevant to ethnic identity in independent Namibia and to relations with Germany.

South African rule and the struggle for independence
South Africa occupied the colony in 1915 after defeating the German force during World War I and administered it as a League of Nations mandate territory from 1919. Although the South African government desired to incorporate 'South-West Africa' into its territory, it never officially did so, although it was administered as the de facto 'fifth province', with the white minority having representation in the whites-only Parliament of South Africa, as well as electing their own local administration the SWA Legislative Assembly. The South African government also appointed the SWA administrator, who had extensive powers.

Following the League's supersession by the United Nations in 1946, South Africa refused to surrender its earlier mandate to be replaced by a United Nations Trusteeship agreement, requiring closer international monitoring of the territory's administration (along with a definite independence schedule). The Herero Chief's Council submitted a number of petitions to the UN calling for it to grant Namibia independence during the 1950s. During the 1960s, when European powers granted independence to their colonies and trust territories in Africa, pressure mounted on South Africa to do so in Namibia. In 1966 the International Court of Justice dismissed a complaint brought by Ethiopia and Liberia against South Africa's continued presence in the territory, but the U.N. General Assembly subsequently revoked South Africa's mandate, while in 1971 the International Court of Justice issued an "advisory opinion" declaring South Africa's continued administration to be illegal.

In response to the 1966 ruling by the International Court of Justice, South-West Africa People's Organisation (SWAPO) military wing, People's Liberation Army of Namibia, a guerrilla group began their armed struggle for independence, but it was not until 1988 that South Africa agreed to end its occupation of Namibia, in accordance with a UN peace plan for the entire region. During the South African occupation of Namibia, white commercial farmers, most of whom came as settlers from South Africa and represented 0.2% of the national population, owned 74% of arable land. Outside the central-southern area of Namibia (known as the "Police Zone" since the German era and which contained the main towns, industries, mines and best arable land), the country was divided into "homelands", the version of South African bantustan applied to Namibia, although only a few were actually established due to non-cooperation by most indigenous Namibians.

After many unsuccessful attempts by the UN to persuade South Africa to agree to the implementation of UN Resolution 435, which had been adopted by the UN Security Council in 1978 as the internationally agreed decolonisation plan for Namibia, transition to independence finally started in 1988 under the tripartite diplomatic agreement between South Africa, Angola and Cuba, with the USSR and the USA as observers, under which South Africa agreed to withdraw and demobilise its forces in Namibia and Cuba agreed to pull back its troops in southern Angola sent to support the MPLA in its war for control of Angola with UNITA. A combined UN civilian and peace-keeping force under Finnish diplomat Martti Ahtisaari supervised the military withdrawals, return of SWAPO exiles and the holding of Namibia's first-ever one-person one-vote election for a constituent assembly in October 1989. This was won by SWAPO although it did not gain the two-thirds majority it had hoped for; the South African-backed Democratic Turnhalle Alliance (DTA) became the official opposition.

Following the adoption of the Namibian Constitution, including entrenched protection for human rights, compensation for state expropriations of private property, an independent judiciary and an executive presidency (the constituent assembly became the national assembly), the country officially became independent on 21 March 1990. Sam Nujoma was sworn in as the first President of Namibia watched by Nelson Mandela (who had been released from prison shortly beforehand) and representatives from 147 countries, including 20 heads of state. Walvis Bay was ceded to Namibia in 1994 upon the end of Apartheid in South Africa.

After independence
Since independence Namibia has successfully completed the transition from white minority apartheid rule to parliamentary democracy. Multiparty democracy was introduced and has been maintained, with local, regional and national elections held regularly. Several registered political parties are active and represented in the National Assembly, although Swapo Party has won every election since independence. The transition from the 15-year rule of President Sam Nujoma to his successor, Hifikepunye Pohamba in 2005 went smoothly.

Namibian government has promoted a policy of national reconciliation and issued an amnesty for those who had fought on either side during the liberation war. The civil war in Angola had a limited impact on Namibians living in the north of the country. In 1998, Namibia Defence Force (NDF) troops were sent to the Democratic Republic of the Congo as part of a Southern African Development Community (SADC) contingent. In August 1999, a secessionist attempt in the northeastern Caprivi region was successfully quashed.

Geography and climate
At 825,418 km2 (318,696 sq mi), Namibia is the world's thirty-fourth largest country (after Venezuela). It lies mostly between latitudes 17° and 29°S (a small area is north of 17°), and longitudes 11° and 26°E.

Namibia is divided into 13 regions and subdivided into 107 constituencies. The administrative division of Namibia is tabled by Delimitation Commissions and accepted or declined by the National Assembly. Since state foundation three Delimitation Commissions have been formed, the last one in 2002 under the chairmanship of Peter Shivute. Regional councillors are directly elected through secret ballots (regional elections) by the inhabitants of their constituencies.

Geographical areas
The Namibian landscape consists generally of five geographical areas, each with characteristic abiotic conditions and vegetation with some variation within and overlap between them: the Central Plateau, the Namib Desert, the Great Escarpment, the Bushveld, and the Kalahari Desert.

The Central Plateau runs from north to south, bordered by the Skeleton Coast to the northwest, the Namib Desert and its coastal plains to the southwest, the Orange River to the south, and the Kalahari Desert to the east. The Central Plateau is home to the highest point in Namibia at Königstein elevation 2,606 meters (8,550 ft). Within the wide, flat Central Plateau is the majority of Namibia’s population and economic activity. Windhoek, the nation’s capital, is located here, as well as most of the arable land. Although arable land accounts for only 1% of Namibia, nearly half of the population is employed in agriculture.

The abiotic conditions here are similar to those found along the Escarpment; however the topographic complexity is reduced. Summer temperatures in the area can reach 40 °C (104 °F), and frosts are common in the winter.

 Namib Desert

Namib Desert
The Namib Desert is a broad expanse of hyper-arid gravel plains and dunes that stretches along Namibia's entire coastline. It varies between 100 to many hundreds of kilometres in width. Areas within the Namib include the Skeleton Coast and the Kaokoveld in the north and the extensive Namib Sand Sea along the central coast. The sands that make up the sand sea result from processes of erosion that take place in the Orange River valley and areas further to the south. As sand-laden waters drop their suspended loads into the Atlantic, onshore currents deposit them along the shore. The prevailing south west winds then pick up and redeposit the sand in the form of massive dunes in the widespread sand sea, forming the largest sand dunes in the world. In areas where the supply of sand is reduced because of the inability of the sand to cross riverbeds, the winds also scour the land to form large gravel plains. In many areas of the Namib Desert there is little vegetation aside from lichens found in the gravel plains and in dry river beds where plants can access subterranean water.

 Namib Escarpment

Great Escarpment
The Great Escarpment swiftly rises to over 2,000 meters (6,562 ft). Average temperatures and temperature ranges increase further inland from the cold Atlantic waters, while the lingering coastal fogs slowly diminish. Although the area is rocky with poorly developed soils, it is nonetheless significantly more productive than the Namib Desert. As summer winds are forced over the Escarpment, moisture is extracted as precipitation. The water, along with rapidly changing topography, is responsible for the creation of microhabitats which offer a wide range of organisms, many of them endemic. Vegetation along the escarpment varies in both form and density, with community structure ranging from dense woodlands to more shrubby areas with scattered trees. A number of Acacia species are found here, as well as grasses and other shrubby vegetation.

Bushveld
The Bushveld is found in north eastern Namibia along the Angolan border and in the Caprivi Strip which is the vestige of a narrow corridor demarcated for the German Empire to access the Zambezi River. The area receives a significantly greater amount of precipitation than the rest of the country, averaging around 400 mm (15.7 in) per year. Temperatures are also cooler and more moderate, with approximate seasonal variations of between 10 and 30 °C (50 and 86 °F). The area is generally flat and the soils sandy, limiting their ability to retain water. Located adjacent to the Bushveld in north-central Namibia is one of nature’s most spectacular features: the Etosha Pan. For most of the year it is a dry, saline wasteland, but during the wet season, it forms a shallow lake covering more than 6,000 square kilometres (2,317 sq mi). The area is ecologically important and vital to the huge numbers of birds and animals from the surrounding savannah that gather in the region as summer drought forces them to the scattered waterholes that ring the pan. The Bushveld area has been demarcated by the World Wildlife Fund as part of the Angolan Mopane woodlands ecoregion, which extends north across the Cunene River into neighbouring Angola.

 The Kalahari Desert

Kalahari Desert
The Kalahari Desert is perhaps Namibia’s best known geographical feature. Shared with South Africa and Botswana, it has a variety of localized environments ranging from hyper-arid sandy desert, to areas that seem to defy the common definition of desert. One of these areas, known as the Succulent Karoo, is home to over 5,000 species of plants, nearly half of them endemic; fully one third of the world’s succulents are found in the Karoo.

The reason behind this high productivity and endemism may be the relatively stable nature of precipitation. The Karoo apparently does not experience drought on a regular basis, so even though the area is technically desert, regular winter rains provide enough moisture to support the region’s interesting plant community. Another feature of the Kalahari, indeed many parts of Namibia, are inselbergs, isolated mountains that create microclimates and habitat for organisms not adapted to life in the surrounding desert matrix.

Coastal Desert
Namibia’s Coastal Desert is one of the oldest deserts in the world. Its sand dunes, created by the strong onshore winds, are the highest in the world.

The Namib Desert and the Namib-Naukluft National Park are located here. The Namibian coastal deserts are one of the richest sources of diamonds on earth. The area is divided into the northern Skeleton Coast and the southern Diamond Coast. Because of the location of the shoreline— at the point where the Atlantic's cold water reach Africa— there is often extremely dense fog.

Sandy beach composes 54% of the shoreline, and mixed sand and rock form another 28%. Only 16% of the total length is rocky shoreline. The coastal plains are "dune fields", gravel plains covered with lichen and some scattered salt pans. Near the coast there are areas where the dunes are vegetated with hammocks. Namibia has rich coastal and marine resources that remain largely unexplored.

Weather and climate
Namibia has more than 300 days of sunshine per year. It is situated at the southern edge of the tropics; the Tropic of Capricorn cuts the country about in half. The winter (June – August) is generally dry, both rainy seasons occur in summer, the small rainy season between September and November, the big one between February and April. Humidity is low, and average rainfall varies from almost zero in the coastal desert to more than 600 mm in the Caprivi Strip. Rainfall is however highly variable, and droughts are common. The last bad rainy season with rainfall far below the annual average occurred in summer 2006/07.

Weather and climate in the coastal area are dominated by the cold, north-flowing Benguela current of the Atlantic Ocean which accounts for very low precipitation (50 mm per year or less), frequent dense fog, and overall lower temperatures than in the rest of the country. In Winter, occasionally a condition known as Bergwind (German: Mountain breeze) or Oosweer (Afrikaans: East weather) occurs, a hot dry wind blowing from the inland to the coast. As the area behind the coast is a desert, these winds can develop into sand storms with sand deposits in the Atlantic Ocean visible on satellite images.

The Central Plateau and Kalahari areas have wide diurnal temperature ranges of up to 30C.

Efundja, the annual flooding of the northern parts of the country, often causes not only damage to infrastructure but loss of life. The rains that cause these floods originate in Angola, flow into Namibia's Cuvelai basin, and fill the Oshanas (Oshiwambo: flood plains) there. The worst floods so far occurred in March 2011 and displaced 21,000 people.