Geology Of Namibia
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Geology Of Namibia
The geology of Namibia encompasses rocks of Paleoproterozoic, Mesoproterozoic and Neoproterozoic and Paleozoic to Cenozoic age. About 46% of the countryʼs surface are bedrock exposure, while the remainder is covered by the young overburden sediments of the Kalahari and Namib deserts. The country is famous for its mineral deposits of Tsumeb, as well as many geological sites of interest, from paleontological, geomorphological and volcanic character. Due to the exposure of the formations in a desert climate and the former German colony, the geology of Namibia is relatively well studied compared to the more tropical less exposed northern neighbors. Stratigraphy and tectonics Large areas of the Namibian geology exposed onshore are associated with the Late Proterozoic Pan-African orogenic cycle.Kukulus, 2004, p.10 The geology of Namibia is dominated in the north by metasediments of the Neoproterozoic Damara Belt (or Namibian System), while in the south large areas are underlain by ...
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Metasediment
In geology, metasedimentary rock is a type of metamorphic rock. Such a rock was first formed through the deposition and solidification of sediment Sediment is a naturally occurring material that is broken down by processes of weathering and erosion, and is subsequently transported by the action of wind, water, or ice or by the force of gravity acting on the particles. For example, sand an .... Then, the rock was buried underneath subsequent rock and was subjected to high pressures and temperatures, causing the rock to recrystallize. The overall composition of a metasedimentary rock can be used to identify the original sedimentary rock, even where they have been subject to high-grade metamorphism and intense deformation. Types of metasedimentary rocks See also * References Metamorphic petrology {{petrology-stub ...
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Congo Craton
The Congo Craton, covered by the Palaeozoic-to-recent Congo Basin, is an ancient Precambrian craton that with four others (the Kaapvaal, Zimbabwe, Tanzania, and West African cratons) makes up the modern continent of Africa. These cratons were formed between about 3.6 and 2.0 billion years ago and have been tectonically stable since that time. All of these cratons are bounded by younger fold belts formed between 2.0 billion and 300 million years ago. The Congo Craton occupies a large part of central southern Africa, extending from the Kasai region of the DRC into Sudan and Angola. It forms parts of the countries of Gabon, Cameroon, and the Central African Republic. A small portion extends into Zambia as well, where it is called the Bangweulu Block. Congo–São Francisco The Congo Craton and the São Francisco Craton are stable Archaean blocks that formed a coherent landmass until the opening of the South Atlantic Ocean during the break-up of Gondwana ( 2000–130 Ma). They ...
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Epupa Complex
Epupa (Herero for "falling waters") may refer to: * Epupa Falls, waterfalls on the border between Angola and Namibia * Epupa Constituency, electoral constituency in north-western Namibia named after the falls * Epupa, Namibia, the settlement at Epupa Falls Epupa Falls (also known as Monte Negro Falls in Angola) is a series of large waterfalls formed by the Cunene River on the border of Angola and Namibia, in the Kaokoland area of the Kunene Region. The river is about wide in this area and drops in ... {{geodis Otjiherero words and phrases ...
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Outjo
Outjo (Otjiherero: ''small hills'') is a city of 6,000 inhabitants in the Kunene Region of Namibia. It is the district capital of Outjo Constituency. It is best known as a main gateway to Etosha National Park. Overview The town was founded by Germans under the command of Colonel Theodor von Leutwein in 1897 as a small military base in order to explore the northern area of German South West Africa. The local historical museum ( Franke Haus Museum) details the campaign of Major Viktor Franke in Ovamboland. The "Naulila monument" commemorates the small expedition on the Portuguese fort of Naulila in Angola by Major Viktor Franke in October 1914 following the massacre of a German delegation which had been sent to negotiate a treaty of non-aggression. it is one of the fast developing town in the Kunene Region. South of Outjo is the Ugab River, one of the major rivers of Namibia. The town lies near Gamkarab Cave, known for its stalactites and stalagmites and its pietersite. The ...
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Metamorphic Rock
Metamorphic rocks arise from the transformation of existing rock to new types of rock in a process called metamorphism. The original rock (protolith) is subjected to temperatures greater than and, often, elevated pressure of or more, causing profound physical or chemical changes. During this process, the rock remains mostly in the solid state, but gradually recrystallizes to a new texture or mineral composition. The protolith may be an igneous, sedimentary, or existing metamorphic rock. Metamorphic rocks make up a large part of the Earth's crust and form 12% of the Earth's land surface. They are classified by their protolith, their chemical and mineral makeup, and their texture. They may be formed simply by being deeply buried beneath the Earth's surface, where they are subject to high temperatures and the great pressure of the rock layers above. They can also form from tectonic processes such as continental collisions, which cause horizontal pressure, friction, and distorti ...
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Epupa Metamorphic Complex
Epupa (Herero for "falling waters") may refer to: * Epupa Falls, waterfalls on the border between Angola and Namibia * Epupa Constituency, electoral constituency in north-western Namibia named after the falls * Epupa, Namibia, the settlement at Epupa Falls Epupa Falls (also known as Monte Negro Falls in Angola) is a series of large waterfalls formed by the Cunene River on the border of Angola and Namibia, in the Kaokoland area of the Kunene Region. The river is about wide in this area and drops in ... {{geodis Otjiherero words and phrases ...
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Kunene River
The Cunene (Portuguese spelling) or Kunene (common Namibian spelling) is a river in Southern Africa. It flows from the Angola highlands south to the border with Namibia. It then flows west along the border until it reaches the Atlantic Ocean. It is one of the few perennial rivers in the region. It is about long, with a drainage basin in area. Its mean annual discharge is 174 m3/s (6,145 cfs) at its mouth. The Epupa Falls lie on the river. Olushandja Dam dams a tributary of the river, the Etaka, and helps provide the Ruacana Power Station with water. Dam controversies The Namibian government proposed in the late 1990s to build the Epupa Dam, a controversial hydroelectric dam on the Cunene. In 2012 the Governments of Namibia and Angola announced plans to jointly build the Orokawe dam in the Baynes Mountains. According to the indigenous Himba who would have been most affected by the construction of the dam, the dam threatens the local ecosystem and therefore the economic bas ...
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Basement (geology)
In geology, basement and crystalline basement are crystalline rocks lying above the mantle and beneath all other rocks and sediments. They are sometimes exposed at the surface, but often they are buried under miles of rock and sediment. The basement rocks lie below a sedimentation, sedimentary platform (geology), platform or cover, or more generally any rock below sedimentary rocks or sedimentary basins that are metamorphic rock, metamorphic or Igneous rock, igneous in origin. In the same way, the sediments or sedimentary rocks on top of the basement can be called a "cover" or "sedimentary cover". Crustal rocks are modified several times before they become basement, and these transitions alter their composition. Continental crust Basement rock is the thick foundation of ancient, and oldest, metamorphic and igneous rock that forms the Crust (geology), crust of continents, often in the form of granite. Basement rock is contrasted to overlying sedimentary rocks which are laid down ...
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