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Namibia is an amazing country in the south west of Africa and offers wonderful wildlife viewing cultural experiences and vast landscapes. With Africa Book Direct you can contact hotels lodges and places to stay in Namibia direct making reservations with accommdodation and finding out all the information you need about self catering camping sites hotels guesthouses and lodges in Namibia. Is your accommodation listed? If not please contact us
Namibia is a large and beautiful desert country on the South west coast of Africa. Namibia has fascinating geography, history, cultural and wildlife, making Namibia a wonderful place for an exciting holiday. Namibia is predominantly a desert country with approx 310 days of sunshine each year and Namibia is often referred to as the land of contrast with breathtaking mountains, deserts, amazing wildlife and fascinating culture. Memories of Namibia will forever remain in your heart.
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.
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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
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
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.
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 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
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.
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[update] 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[update] occurred in March 2011 and displaced 21,000 people.
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