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Hanglip
Hanglip (Afrikaans for ''hanging lip'', Venda: Songozwi'), thavha ya VhaDzanani is a prominent mountain peak near Louis Trichardt, South Africa. It is situated in the Vhembe District of Limpopo in the central Soutpansberg range. The peak with radar station, at 1,719 meters a.s.l., forms a conspicuous landmark visible from the town and the N1 national road. Hanglip mountain is situated in the 354 hectare Hanglip Forest Reserve within the Hanglip State Forest. The state forest contains commercial pine plantations, protected natural forest and bushveld. The pine plantations are harvested in 30 to 40 year cycles for construction wood. Geologically the mountain consists of tilted layers of the Karoo succession including glacial till deposits. Red quartzite deposits and grey andesite Andesite () is a volcanic rock of intermediate composition. In a general sense, it is the intermediate type between silica-poor basalt and silica-rich rhyolite. It is fine-grained (aphanitic) to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Soutpansberg
The Soutpansberg, (formerly ''Zoutpansberg'') meaning "Salt Pan Mountain" in Afrikaans, is a Mountain range, range of mountains in far northern South Africa. It is located in Vhembe District Municipality, Vhembe District, Limpopo. It is named for the Salt pan (geology), salt pan ( ve, Thavha ya muno, or "place of salt") located at its western end. The mountain range reaches the opposite extremity in the Matikwa Nature Reserve, some due east. The range as a whole had no Venda language, Venda name, as it was instead known by its sub-ranges which include Dzanani, Hanglip, Songozwi and others. Of late it is however known as Tha vhani ya muno, meaning "mountain of salt". The Soutpansberg forms part of the 'Vhembe Biosphere Reserve', which was designated as a biosphere reserve by UNESCO in 2009. The latter reserve also includes the Blouberg Range, Kruger National Park, Makgabeng Plateau, Makuleke Wetlands and the Mapungubwe Cultural Landscape. Geography The mountain is intersected by t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Mountains In South Africa
List of Mountains in South Africa, Lesotho and Eswatini is a general list of mountains in South Africa, Lesotho and Eswatini with elevation. This list includes mountains in two other sovereign states, in the Stormberg-Drakensberg range, where the highest elevations are to be found in Lesotho, as well as Emlembe, the highest mountain in Eswatini, located at the border with South Africa. The highest mountain in South Africa is high Mafadi, located on the border of South Africa and Lesotho. Several of the highest peaks have snow in the Southern hemisphere winter season. A ''Khulu'' is a peak above and not within of another ''Khulu'', as defined by the Mountain Club of South Africa. Seweweekspoortpiek and Du Toits Peak are among the ultra prominent peaks of Africa. A few mountains, such as Spion Kop or Isandlwana are historically important hills, even though they are relatively not very high. Table Mountain is important because of its emblematic flatness. List See also ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schoemansdal, Limpopo
Schoemansdal (Dutch for ''Schoeman's dale''; at first Oude Dorp and Zoutpansbergdorp) was a settlement situated 16 km west of Louis Trichardt (Makhado), which had its origins during the Great Trek. It existed from 1848 to 1867, and functioned as the capital of an autonomous region until the S.A.R. Volksraad was established, when the outpost came under the supervision and regulations of the central government. The settlement was evacuated after only thirty years when attacked by Venda militants. The government rendered indecisive support and the town as torched by Katze-Katze on the night of 15 July 1867. After the S.A.R. reestablished control over the area in 1898, the former settlement was ignored and a new one started, at the present Louis Trichardt. Consequently Schoemansdal was the only Voortrekker settlement not to evolve into a modern town. The archaeological site with traces of the former settlement is currently state property and access is controlled. It is situate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Till
image:Geschiebemergel.JPG, Closeup of glacial till. Note that the larger grains (pebbles and gravel) in the till are completely surrounded by the matrix of finer material (silt and sand), and this characteristic, known as ''matrix support'', is diagnostic of till. image:Glacial till exposed in roadcut-750px.jpg, Glacial till with tufts of grass Till or glacial till is unsorted glacier, glacial sediment. Till is derived from the erosion and entrainment of material by the moving ice of a glacier. It is deposited some distance down-ice to form terminal, lateral, medial and ground moraines. Till is classified into primary deposits, laid down directly by glaciers, and secondary deposits, reworked by fluvial transport and other processes. Description Till is a form of '' glacial drift'', which is rock material transported by a glacier and deposited directly from the ice or from running water emerging from the ice. It is distinguished from other forms of drift in that it is depos ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of South Africa
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 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 isolated summits, but most occur in mountain ranges. Mountains are formed through 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 slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Protected Area
Protected areas or conservation areas are locations which receive protection because of their recognized natural, ecological or cultural values. There are several kinds of protected areas, which vary by level of protection depending on the enabling laws of each country or the regulations of the international organizations involved. Generally speaking though, protected areas are understood to be those in which human presence or at least the exploitation of natural resources (e.g. firewood, non-timber forest products, water, ...) is limited. The term "protected area" also includes marine protected areas, the boundaries of which will include some area of ocean, and transboundary protected areas that overlap multiple countries which remove the borders inside the area for conservation and economic purposes. There are over 161,000 protected areas in the world (as of October 2010) with more added daily, representing between 10 and 15 percent of the world's land surface area. As of 20 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kraal
Kraal (also spelled ''craal'' or ''kraul'') is an Afrikaans and Dutch word, also used in South African English, for an enclosure for cattle or other livestock, located within a Southern African settlement or village surrounded by a fence of thorn-bush branches, a palisade, mud wall, or other fencing, roughly circular in form. It is similar to a '' boma'' in eastern or central Africa. In Curaçao, another Dutch colony, the enclosure was called "koraal" which in Papiamentu is translated "kura" (still in use today for any enclosed terrain, like a garden). Etymology In the Afrikaans language a ''kraal'' is a term derived from the Portuguese word , cognate with the Spanish-language , which entered into English separately. In Eastern and Central Africa, the equivalent word for a livestock enclosure is '' boma'', but this has taken on wider meanings. In some Southern African regions, the term Kraal is used in Scouting to refer to the team of Scout Leaders of a group. Homestead Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dzanani
Dzanani is a town and also the name of a region in the former Venda, now part of Limpopo province in South Africa. Dzanani was named after MuDzanani, which is one of the main surnames in Venda; and also the then Paramount Chiefs (Khosi Khulu) of Songozwi. The language predominantly spoken is TshiVenda, which is one of the eleven official languages of South Africa. Dzanani is from the town of Thohoyandou, from Louis Trichardt, from Pretoria and about from Harare in Zimbabwe. It is from Polokwane International Airport and about from O. R. Tambo International Airport in Johannesburg. There is a tarred road leading to Dzanani and other nearby areas. It is usually a warm place, but can get very hot in summer and cold in winter. Dzanani used to be one of the four districts in the former Republic of Venda, along with Vuwani, Mutale and Thohoyandou. The Dzata ruins was declared a national heritage site of South Africa.http://www.sahra.org.za/sahris/sites/925040001 The whole of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Venda People
The Venḓa (VhaVenḓa or Vhangona) are a Southern African Bantu people living mostly near the South African-Zimbabwean border. The history of the Venda starts from the Kingdom of Mapungubwe (9th Century) where King Shiriyadenga was the first king of Venda and Mapungubwe. The Mapungubwe Kingdom stretched from the Soutpansberg in the south, across the Limpopo River to the Matopos in the north. The Kingdom declined from 1240, and power moved north to the Great Zimbabwe Kingdom. The first Venda settlement in the Soutpansberg was that of the legendary chief Thoho-ya-Ndou (Head of the Elephant). His royal kraal was called D’zata; its remains have been declared a National Monument. The Mapungubwe Collection is a museum collection of artefacts found at the archaeological site and is housed in the Mapungubwe Museum in Pretoria. Venda people share ancestry with Lobedu people and Kalanga people. They are also related to Sotho-Tswana peoples Sotho-Tswana and Shona groups. All these t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Andesite
Andesite () is a volcanic rock of intermediate composition. In a general sense, it is the intermediate type between silica-poor basalt and silica-rich rhyolite. It is fine-grained (aphanitic) to porphyritic in texture, and is composed predominantly of sodium-rich plagioclase plus pyroxene or hornblende. Andesite is the extrusive equivalent of plutonic diorite. Characteristic of subduction zones, andesite represents the dominant rock type in island arcs. The average composition of the continental crust is andesitic. Along with basalts, andesites are a component of the Martian crust. The name ''andesite'' is derived from the Andes mountain range, where this rock type is found in abundance. It was first applied by Christian Leopold von Buch in 1826. Description Andesite is an aphanitic (fine-grained) igneous rock that is intermediate in its content of silica and low in alkali metals. It has less than 20% quartz and 10% feldspathoid by volume, with at least 65% of the fe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karoo Ice Age
The late Paleozoic icehouse, also known as the Late Paleozoic Ice Age (LPIA) and formerly known as the Karoo ice age, was an ice age that began in the Late Devonian and ended in the Late Permian, occurring from 360 to 255 million years ago (Mya), and large land-based ice-sheets were then present on Earth's surface. It was the second major icehouse period of the Phanerozoic. It is named after the tillite ( Dwyka Group) found in the Karoo Basin of western South Africa, where evidence for the ice age was first clearly identified in the 19th century. The tectonic assembly of the continents of Euramerica and Gondwana into Pangaea, in the Hercynian- Alleghany Orogeny, made a major continental land mass within the Antarctic region, and the closure of the Rheic Ocean and Iapetus Ocean saw disruption of warm-water currents in the Panthalassa Ocean and Paleotethys Sea and an increase in carbon sequestration via silicate weathering, which led to progressive cooling of summers, and the snow ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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