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Maloti Mountains
The Maloti Mountains are a mountain range of the highlands of the Kingdom of Lesotho. They extend for about 100 km into the South African Free State. The Maloti Range is part of the Drakensberg system that includes ranges across large areas of South Africa. “Maloti” is also the plural for Loti, the currency of the Kingdom of Lesotho. The range forms the northern portion of the boundary between the Butha-Buthe District in Lesotho and South Africa's Free State.Zunckel, Kevan. 2010. Connectivity Conservation Management: A Global Guide (with Particular Reference to Mountain Connectivity Conservation). Earthscan. p.77-79 Physiography The range forms a high alpine basalt plateau up to in height. It is located between Butha-Buthe District in Lesotho and the Free State Province of South Africa. The highest point, high Thabana Ntlenyana, is located in the north-east of the range. It is the highest peak of Southern Africa, and the highest in Africa south of the Kilimanjaro. T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thabana Ntlenyana
Thabana Ntlenyana, which literally means "Beautiful little mountain" in Sesotho, is the highest point in Lesotho and the highest mountain in southern Africa. It is situated on the Mohlesi ridge of the Drakensberg/Maloti Mountains, north of Sani Pass. It stands at high. The peak is usually climbed by groups completing a Grand Traverse of the Drakensberg, although the peak is technically in the Maloti Mountains. The peak is often also climbed from Sani Top Chalet or from Vergelegen Nature Reserve. Resources Fresh Water Ecoregions of the WorldGuided Trekking of Thabana Ntlenyana References [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Butha-Buthe District
Butha-Buthe is a Districts of Lesotho, district of Lesotho. Butha-Buthe is the capital or Camptown (Lesotho), camptown, and only town in the district. In the north, Butha-Buthe borders on the Free State (South African province), Free State Province of South Africa. Domestically, it borders on Mokhotlong District in southeast and Leribe District on the south. As of 2014, the district had a population of 118,242 which was 5.88 per cent of the total population of the country. The total area of the district was 1,767 which was 5.82 per cent of the total area of the country. As of 2008, there were 49 per cent economically active people in the district. There were totally 71,012 employed people out of a total of 154,384 people in the district above 15 years of age. The total area planted in 2009 was 7,164 which formed 1.77 per cent of the total area planted in the country. Demographics As of 2014, the district had a population of 118,242, 5.88 per cent of the population of the country ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tugela River
The Tugela River ( zu, Thukela; af, Tugelarivier) is the largest river in KwaZulu-Natal Province, South Africa. With a total length of , it is one of the most important rivers of the country. The river originates in Mont-aux-Sources of the Drakensberg Mountains at an elevation of almost 11,000 feet This has a very detailed description of the river's course. and plunges 947 metres down the Tugela Falls. The Mont-aux-Sources is also the origin of tributaries of two other major South African rivers, the Orange River, Orange and the Vaal River, Vaal. From the Drakensberg range, the Tugela follows a route through the KwaZulu-Natal midlands before flowing into the Indian Ocean. The total catchment area is approximately . Land uses in the catchment are mainly rural subsistence farming and commercial forestry. Tributaries The Tugela has a number of tributaries coming off the Drakensberg, the largest being the Buffalo River (KwaZulu-Natal), Mzinyathi ("Buffalo") River (rising near Maj ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Snow
Snow comprises individual ice crystals that grow while suspended in the atmosphere—usually within clouds—and then fall, accumulating on the ground where they undergo further changes. It consists of frozen crystalline water throughout its life cycle, starting when, under suitable conditions, the ice crystals form in the atmosphere, increase to millimeter size, precipitate and accumulate on surfaces, then metamorphose in place, and ultimately melt, slide or sublimate away. Snowstorms organize and develop by feeding on sources of atmospheric moisture and cold air. Snowflakes nucleate around particles in the atmosphere by attracting supercooled water droplets, which freeze in hexagonal-shaped crystals. Snowflakes take on a variety of shapes, basic among these are platelets, needles, columns and rime. As snow accumulates into a snowpack, it may blow into drifts. Over time, accumulated snow metamorphoses, by sintering, sublimation and freeze-thaw. Where the climate is co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Snow Capped Maloti Mountains - Panoramio
Snow comprises individual ice crystals that grow while suspended in the atmosphere—usually within clouds—and then fall, accumulating on the ground where they undergo further changes. It consists of frozen crystalline water throughout its life cycle, starting when, under suitable conditions, the ice crystals form in the atmosphere, increase to millimeter size, precipitate and accumulate on surfaces, then metamorphose in place, and ultimately melt, slide or sublimate away. Snowstorms organize and develop by feeding on sources of atmospheric moisture and cold air. Snowflakes nucleate around particles in the atmosphere by attracting supercooled water droplets, which freeze in hexagonal-shaped crystals. Snowflakes take on a variety of shapes, basic among these are platelets, needles, columns and rime. As snow accumulates into a snowpack, it may blow into drifts. Over time, accumulated snow metamorphoses, by sintering, sublimation and freeze-thaw. Where the climate is col ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Orange River
The Orange River (from Afrikaans/Dutch: ''Oranjerivier'') is a river in Southern Africa. It is the longest river in South Africa. With a total length of , the Orange River Basin extends from Lesotho into South Africa and Namibia to the north. It rises in the Drakensberg mountains in Lesotho, flowing westwards through South Africa to the Atlantic Ocean. The river forms part of the international borders between South Africa and Lesotho and between South Africa and Namibia, as well as several provincial borders within South Africa. Except for Upington, it does not pass through any major cities. The Orange River plays an important role in the South African economy by providing water for irrigation and hydroelectric power. The river was named the Orange River in honour of the Dutch ruling family, the House of Orange, by the Dutch explorer Robert Jacob Gordon. Other names include simply the word for river, in Khoekhoegowab orthography written as !Garib, which is rendered in Afrikaan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Senqu River
The Orange River (from Afrikaans/Dutch: ''Oranjerivier'') is a river in Southern Africa. It is the longest river in South Africa. With a total length of , the Orange River Basin extends from Lesotho into South Africa and Namibia to the north. It rises in the Drakensberg mountains in Lesotho, flowing westwards through South Africa to the Atlantic Ocean. The river forms part of the international borders between South Africa and Lesotho and between South Africa and Namibia, as well as several provincial borders within South Africa. Except for Upington, it does not pass through any major cities. The Orange River plays an important role in the South African economy by providing water for irrigation and hydroelectric power. The river was named the Orange River in honour of the Dutch ruling family, the House of Orange, by the Dutch explorer Robert Jacob Gordon. Other names include simply the word for river, in Khoekhoegowab orthography written as !Garib, which is rendered in Afrikaa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especially quartz and calcite.Blatt, Harvey and Robert J. Tracy (1996) ''Petrology: Igneous, Sedimentary and Metamorphic'', 2nd ed., Freeman, pp. 281–292 Shale is characterized by its tendency to split into thin layers ( laminae) less than one centimeter in thickness. This property is called '' fissility''. Shale is the most common sedimentary rock. The term ''shale'' is sometimes applied more broadly, as essentially a synonym for mudrock, rather than in the more narrow sense of clay-rich fissile mudrock. Texture Shale typically exhibits varying degrees of fissility. Because of the parallel orientation of clay mineral flakes in shale, it breaks into thin layers, often splintery and usually parallel to the otherwise indistinguishable beddin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bioregion
A bioregion is an ecologically and geographically defined area that is smaller than a biogeographic realm, but larger than an ecoregion or an ecosystem, in the World Wide Fund for Nature classification scheme. There is also an attempt to use the term in a rank-less generalist sense, similar to the terms "biogeographic area" or "biogeographic unit". It may be conceptually similar to an ecoprovince. It is also differently used in the environmentalist context, being coined by Berg and Dasmann (1977). WWF bioregions The World Wide Fund for Nature (WWF) scheme divides some of the biogeographic realms into bioregions, defined as "geographic clusters of ecoregions that may span several habitat types, but have strong biogeographic affinities, particularly at taxonomic levels higher than the species level (genus, family)." The WWF bioregions are as follows: * Afrotropical realm **Western Africa and Sahel **Central Africa **Eastern and Southern Africa ** Horn of Africa **Madagascar–I ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kilimanjaro
Mount Kilimanjaro () is a dormant volcano in Tanzania. It has three volcanic cones: Kibo, Mawenzi, and Shira. It is the highest mountain in Africa and the highest free-standing mountain above sea level in the world: above sea level and about above its plateau base. It is the highest volcano in Africa and the Eastern Hemisphere. Kilimanjaro is the fourth most topographically prominent peak on Earth. It is part of Kilimanjaro National Park and is a major hiking and climbing destination. Because of its shrinking glaciers and ice fields, which are projected to disappear between 2025 and 2035, it has been the subject of many scientific studies. Toponymy The origin of the name Kilimanjaro is not known, but a number of theories exist. European explorers had adopted the name by 1860 and reported that Kilimanjaro was the mountain's Kiswahili name. The 1907 edition of ''The Nuttall Encyclopædia'' also records the name of the mountain as Kilima-Njaro. Johann Ludwig Krapf ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Africa
Africa is the world's second-largest and second-most populous continent, after Asia in both cases. At about 30.3 million km2 (11.7 million square miles) including adjacent islands, it covers 6% of Earth's total surface area and 20% of its land area.Sayre, April Pulley (1999), ''Africa'', Twenty-First Century Books. . With billion people as of , it accounts for about of the world's human population. Africa's population is the youngest amongst all the continents; the median age in 2012 was 19.7, when the worldwide median age was 30.4. Despite a wide range of natural resources, Africa is the least wealthy continent per capita and second-least wealthy by total wealth, behind Oceania. Scholars have attributed this to different factors including geography, climate, tribalism, colonialism, the Cold War, neocolonialism, lack of democracy, and corruption. Despite this low concentration of wealth, recent economic expansion and the large and young population make Afr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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