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Naukluft
The Naukluft Mountains (Afrikaans and German: ''Naukluftberge'') are a mountain range in central Namibia. The southern part of the mountain range forms the easternmost part of the Namib-Naukluft National Park. The northern mountains are occupied by privately held farms. They are known for their wildlife, including mountain zebras and leopards. The mountains have many small streams and waterfalls. ''Naukluft'' is the Namibian German rendering of the Afrikaans , meaning "narrow ravine", from ('narrow', cf Dutch ) and ('ravine', cf German ). Geology The Naukluft Mountains are a nappe complex: a stack of rock units which have been transported toward the southeast on a basal thrust fault. The first geological maps and cross-sections of the mountain range were made in the 1930s by Henno Martin and Hermann Korn. The rocks are interbedded sediments, dominated by dolomites, quartzites and shales, deposited in a shallow marine environment in the hinterland of the Damara orogeny betwee ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Namib-Naukluft National Park
The Namib-Naukluft Park is a national park in western Namibia, situated between the coast of the Atlantic Ocean and the edge of the Great Escarpment. It encompasses part of the Namib Desert (considered the world's oldest desert), the Naukluft mountain range, and the lagoon at Sandwich Harbour. The best-known area of the park and one of the main visitor attractions in Namibia is Sossusvlei, a clay pan surrounded by dunes, and Sesriem, a small canyon of the Tsauchab. The desert research station of Gobabeb is situated within the park. Location and description With an overall area of , the Namib-Naukluft National Park was at the time of its last expansion the largest game park in Africa and the fourth largest in the world. It consists of a strip of land on the Atlantic Ocean, including of sea, that extends roughly north-to-south from the Swakop River to the B4 road to Lüderitz. Wildlife A surprising collection of creatures survives in the hyper-arid region, including snakes, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Naukluft Waterkloof
The Naukluft Mountains (Afrikaans and German: ''Naukluftberge'') are a mountain range in central Namibia. The southern part of the mountain range forms the easternmost part of the Namib-Naukluft National Park. The northern mountains are occupied by privately held farms. They are known for their wildlife, including mountain zebras and leopards. The mountains have many small streams and waterfalls. ''Naukluft'' is the Namibian German rendering of the Afrikaans , meaning "narrow ravine", from ('narrow', cf Dutch ) and ('ravine', cf German ). Geology The Naukluft Mountains are a nappe complex: a stack of rock units which have been transported toward the southeast on a basal thrust fault. The first geological maps and cross-sections of the mountain range were made in the 1930s by Henno Martin and Hermann Korn. The rocks are interbedded sediments, dominated by dolomites, quartzites and shales, deposited in a shallow marine environment in the hinterland of the Damara orogeny betwee ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Naukluft Von Sesriem Aus Gesegehen
The Naukluft Mountains (Afrikaans and German: ''Naukluftberge'') are a mountain range in central Namibia. The southern part of the mountain range forms the easternmost part of the Namib-Naukluft National Park. The northern mountains are occupied by privately held farms. They are known for their wildlife, including mountain zebras and leopards. The mountains have many small streams and waterfalls. ''Naukluft'' is the Namibian German rendering of the Afrikaans , meaning "narrow ravine", from ('narrow', cf Dutch ) and ('ravine', cf German ). Geology The Naukluft Mountains are a nappe complex: a stack of rock units which have been transported toward the southeast on a basal thrust fault. The first geological maps and cross-sections of the mountain range were made in the 1930s by Henno Martin and Hermann Korn. The rocks are interbedded sediments, dominated by dolomites, quartzites and shales, deposited in a shallow marine environment in the hinterland of the Damara orogeny betwee ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Namibian Savanna Woodlands
The Namibian savanna woodlands, also known as the Namib escarpment woodlands, are deserts and xeric shrublands ecoregion of Namibia and Angola. Geography They extend north and south from southwestern Angola to central Namibia, east of the coastal Namib Desert. The woodlands cover the Namib escarpment, which rises from the low-lying Namib coastal plain to the Southern African plateau on the east. Baynes (2038 m), Erongo (2319 m), Naukluft (1974 m), Spitzkoppe (1759 m), and Gamsberg (2347 m) mountains lie along the edge of the escarpment. Brandberg Mountain (257 m) lies west of the escarpment in the Namib Desert, and is included in the ecoregion.Burgess, Neil, Jennifer D'Amico Hales, Emma Underwood, et al. (2004). ''Terrestrial Ecoregions of Africa and Madagascar: A Conservation Assessment''. World Wildlife Fund. Island Press, 2004. To the northeast lie more humid woodland and savanna ecoregions – the Angolan miombo woodlands at furthest northern end, and the Angolan mopane woodl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Damara Orogeny
The Damara orogeny was part of the Pan-African orogeny. The Damara orogeny occurred late in the creation of Gondwana, at the intersection of the Congo and the Kalahari cratons.; ; ; ; The Damara orogeny involved the suturing of the Congo– São Francisco and Río de la Plata cratons at 580–550 Ma (together with India forming northern Gondwana) before the amalgamation of the Kalahari and Mawson cratons in the Kuunga–Damara orogeny at 530 Ma (southern Gondwana). The Adamastor Ocean closed southwards from the Araçuaı́ Belt (São Francisco Craton, now in South America) to the Kaoko Belt (Congo Craton, now in Africa) 580–550 Ma and 545–530 Ma Gariep Belt (Kalahari Craton, now in southern Africa). The Damara orogeny saw a peak in deformation and metamorphism at 530–500 Ma. Thrusting occurred onto the Kalahari Craton until 480 Ma. Río de la Plata docked to Congo before the closure of the Damara Belt oceans (Mozambique and Khomas) whi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Zebra
The mountain zebra (''Equus zebra'') is a zebra species in the family Equidae, native to southwestern Africa. There are two subspecies, the Cape mountain zebra (''E. z. zebra'') found in South Africa and Hartmann's mountain zebra (''E. z. hartmannae'') found in south-western Angola and Namibia. Taxonomy The mountain zebra comprises two subspecies: In 2004, C. P. Groves and C. H. Bell investigated the taxonomy of the zebras (genus ''Equus'', subgenus ''Hippotigris''). They concluded that the mountain zebra (''Equus zebra zebra'') and Hartmann's mountain zebra (''Equus zebra hartmannae'') are distinct, and suggested that the two would be better classified as separate species, ''Equus zebra'' and ''Equus hartmannae''. However, in a sexual genetic study that included 295 mountain zebra specimens, Moodley and Harley (2005) found nothing to support the separation of the two mountain zebra populations into separate species. They concluded that the Cape mountain zebra and Hartmann' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Namibia
Namibia (, ), officially the Republic of Namibia, is a country in Southern Africa. Its western border is the Atlantic Ocean. It shares land borders with Zambia and Angola to the north, Botswana to the east and South Africa to the south and east. Although Kazungula, it does not border Zimbabwe, less than 200 metres (660 feet) of the Botswanan right bank of the Zambezi, Zambezi River separates the two countries. Namibia 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 driest country in sub-Saharan Africa, Namibia has been inhabited since pre-historic times by the San people, San, Damara people, Damara and Nama people. Around the 14th century, immigration, immigrating Bantu peoples arrived as part of the Bantu expansion. Since ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hardap Region
Hardap is one of the fourteen regions of Namibia, its capital is Mariental. Hardap contains the municipality of Mariental, the towns Rehoboth and Aranos, and the self-governed villages Gibeon, Gochas, Kalkrand, Stampriet and Maltahöhe. It is home to the Hardap Dam. Hardap stretches the entire width of Namibia, from the Atlantic Ocean in the west to Namibia's eastern national border. In the northeast, it borders the Kgalagadi District of Botswana, and in the southeast, it borders the Northern Cape Province of South Africa. Domestically, it borders the following regions: *Erongo – northwest *Khomas – north central *Omaheke – northeast * ǁKaras – south Politics As of 2020, Hardap had 52,534 registered voters. The region comprises eight political constituencies: * Gibeon * Mariental Rural * Mariental Urban * Rehoboth Rural * Rehoboth Urban East * Rehoboth Urban West * Aranos (created in 2013) * Daweb (created in 2013) As in all other regions, SWAPO was by far the st ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Ranges Of Namibia
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited Summit (topography), summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Evaporite
An evaporite () is a water-soluble sedimentary mineral deposit that results from concentration and crystallization by evaporation from an aqueous solution. There are two types of evaporite deposits: marine, which can also be described as ocean deposits, and non-marine, which are found in standing bodies of water such as lakes. Evaporites are considered sedimentary rocks and are formed by chemical sediments. Formation of evaporite rocks Although all water bodies on the surface and in aquifers contain dissolved salts, the water must evaporate into the atmosphere for the minerals to precipitate. For this to happen, the water body must enter a restricted environment where water input into this environment remains below the net rate of evaporation. This is usually an arid environment with a small basin fed by a limited input of water. When evaporation occurs, the remaining water is enriched in salts, and they precipitate when the water becomes supersaturated. Evaporite depositi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Klippe
350px, Schematic overview of a thrust system. The shaded material is called a window_(geology).html"_;"title="nappe._The_erosional_hole_is_called_a__window_(geology)">window_or_fenster._The_klippe_is_the_isolated_block_of_the_nappe_overlying_autochthonous_material. A_klippe_(German_language.html" "title="window (geology)">window or fenster. The klippe is the isolated block of the nappe overlying autochthonous material.">window_(geology).html" ;"title="nappe. The erosional hole is called a window (geology)">window or fenster. The klippe is the isolated block of the nappe overlying autochthonous material. A klippe (German language">German for cliff or crag) is a geological feature of thrust fault terrains. The klippe is the remnant portion of a nappe after erosion has removed connecting portions of the nappe. This process results in an outlier of exotic, often nearly horizontally translated strata overlying autochthonous strata. Examples of klippes include: *Chief Mountain, Mont ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lithologies
The lithology of a rock unit is a description of its physical characteristics visible at outcrop, in hand or core samples, or with low magnification microscopy. Physical characteristics include colour, texture, grain size, and composition. Lithology may refer to either a detailed description of these characteristics, or a summary of the gross physical character of a rock. Examples of lithologies in the second sense include sandstone, slate, basalt, or limestone. Lithology is the basis of subdividing rock sequences into individual lithostratigraphic units for the purposes of mapping and correlation between areas. In certain applications, such as site investigations, lithology is described using a standard terminology such as in the European geotechnical standard Eurocode 7. Rock type The naming of a lithology is based on the rock type. The three major rock types are igneous, sedimentary, and metamorphic. Igneous rocks are formed directly from magma, which is a mixture of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
