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Balancing Rocks
The Balancing Rocks are geomorphological features of igneous rocks found in many parts of Zimbabwe, and are particularly noteworthy in Matopos National Park, and near the township of Epworth, to the southeast of Harare. Notable rocks The Domboremari, also known as the Money Rock, is a formation of three boulders that form part of the Chiremba Balancing Rocks on the northwestern outskirts of Epworth (coordinates: ): this particular rock formation is notable because it appears in all Zimbabwean banknotes issued since 1981, and is also the prominent feature of the logo of the Reserve Bank of Zimbabwe The Reserve Bank of Zimbabwe is the central bank of Zimbabwe and is headquartered in the capital city Harare. History The bank traces its history to the Reserve Bank of Rhodesia, founded on 22 May 1964, but which succeeded the Bank of Rhodesia .... References {{Zimbabwe-struct-stub Harare Landforms of Zimbabwe Rock formations of Africa Geography of Harare Province ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Matopos National Park
The Matobo National Park forms the core of the Matobo or Matopos Hills, an area of granite kopjes and wooded valleys commencing some south of Bulawayo, southern Zimbabwe. The hills were formed over 2 billion years ago with granite being forced to the surface, this has eroded to produce smooth "whaleback dwalas" and broken kopjes, strewn with boulders and interspersed with thickets of vegetation. Matopo/Matob was named by the Lozwi, who are the ancestors of Kalanga. A different tradition states that the first King , Mzilikazi Khumalo when told by the local residents that the great granite domes were called madombo he replied , possible half jest, "We will call them matobo" - an IsiNdebele play on 'Bald heads'. The Hills cover an area of about 3100 km² (1200 sq mi), of which 424 km² (164 sq mi) is National Park, the remainder being largely communal land and a small proportion of commercial farmland. The park extends along the Thuli, Mtshelele, Maleme and M ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Monadnock
An inselberg or monadnock () is an isolated rock hill, knob, ridge, or small mountain that rises abruptly from a gently sloping or virtually level surrounding plain. In Southern Africa a similar formation of granite is known as a koppie, an Afrikaans word ("little head") from the Dutch diminutive word ''kopje''. If the inselberg is dome-shaped and formed from granite or gneiss, it can also be called a bornhardt, though not all bornhardts are inselbergs. An inselberg results when a body of rock resistant to erosion, such as granite, occurring within a body of softer rocks, is exposed by differential erosion and lowering of the surrounding landscape. Etymology Inselberg The word ''inselberg'' is a loan word from German, and means "island mountain". The term was coined in 1900 by geologist Wilhelm Bornhardt (1864–1946) to describe the abundance of such features found in eastern Africa. At that time, the term applied only to arid landscape features. However, it has sin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zimbabwe
Zimbabwe (), officially the Republic of Zimbabwe, is a landlocked country located in Southeast Africa, between the Zambezi and Limpopo Rivers, bordered by South Africa to the south, Botswana to the south-west, Zambia to the north, and Mozambique to the east. The capital and largest city is Harare. The second largest city is Bulawayo. A country of roughly 15 million people, Zimbabwe has 16 official languages, with English, Shona language, Shona, and Northern Ndebele language, Ndebele the most common. Beginning in the 9th century, during its late Iron Age, the Bantu peoples, Bantu people (who would become the ethnic Shona people, Shona) built the city-state of Great Zimbabwe which became one of the major African trade centres by the 11th century, controlling the gold, ivory and copper trades with the Swahili coast, which were connected to Arab and Indian states. By the mid 15th century, the city-state had been abandoned. From there, the Kingdom of Zimbabwe was established, fol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geomorphology
Geomorphology (from Ancient Greek: , ', "earth"; , ', "form"; and , ', "study") is the scientific study of the origin and evolution of topographic and bathymetric features created by physical, chemical or biological processes operating at or near Earth's surface. Geomorphologists seek to understand why landscapes look the way they do, to understand landform and terrain history and dynamics and to predict changes through a combination of field observations, physical experiments and numerical modeling. Geomorphologists work within disciplines such as physical geography, geology, geodesy, engineering geology, archaeology, climatology, and geotechnical engineering. This broad base of interests contributes to many research styles and interests within the field. Overview Earth's surface is modified by a combination of surface processes that shape landscapes, and geologic processes that cause tectonic uplift and subsidence, and shape the coastal geography. Surface processes co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Igneous
Igneous rock (derived from the Latin word ''ignis'' meaning fire), or magmatic rock, is one of the three main rock types, the others being sedimentary and metamorphic. Igneous rock is formed through the cooling and solidification of magma or lava. The magma can be derived from partial melts of existing rocks in either a planet's mantle or crust. Typically, the melting is caused by one or more of three processes: an increase in temperature, a decrease in pressure, or a change in composition. Solidification into rock occurs either below the surface as intrusive rocks or on the surface as extrusive rocks. Igneous rock may form with crystallization to form granular, crystalline rocks, or without crystallization to form natural glasses. Igneous rocks occur in a wide range of geological settings: shields, platforms, orogens, basins, large igneous provinces, extended crust and oceanic crust. Geological significance Igneous and metamorphic rocks make up 90–95% of the top ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Epworth, Zimbabwe
Epworth is a dormitory town in south-eastern Harare Province, Zimbabwe. Its population exploded in the late 1970s and 1980s as an informal settlement. Background Epworth is located about twelve kilometres from the Harare city centre. It is a high-density dormitory town administered by the Epworth Local Board. It is bisected by a stream into two parts. The Balancing Rocks found in the northern approaches of the town are famous, and are featured on all bank notes issued by the Reserve Bank of Zimbabwe. History Epworth Mission was established by the Rev. Shimmin as a Methodist Mission Station more than a century ago, in 1890. Epworth then and to this day is divided into 7 wards. A large influx of people occurred during the late 1970s and early 1980s with the population being 20,000 in 1980 and 35,000 in 1987. The Methodist Church could not control the influx of people, and therefore transferred ownership of the farm to the Ministry of Local Government in 1983. By 2002 the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Harare
Harare (; formerly Salisbury ) is the capital and most populous city of Zimbabwe. The city proper has an area of 940 km2 (371 mi2) and a population of 2.12 million in the 2012 census and an estimated 3.12 million in its metropolitan area in 2019. Situated in north-eastern Zimbabwe in the country's Mashonaland region, Harare is a metropolitan province, which also incorporates the municipalities of Chitungwiza and Epworth. The city sits on a plateau at an elevation of above sea level and its climate falls into the subtropical highland category. The city was founded in 1890 by the Pioneer Column, a small military force of the British South Africa Company, and named Fort Salisbury after the UK Prime Minister Lord Salisbury. Company administrators demarcated the city and ran it until Southern Rhodesia achieved responsible government in 1923. Salisbury was thereafter the seat of the Southern Rhodesian (later Rhodesian) government and, between 1953 and 1963, th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reserve Bank Of Zimbabwe
The Reserve Bank of Zimbabwe is the central bank of Zimbabwe and is headquartered in the capital city Harare. History The bank traces its history to the Reserve Bank of Rhodesia, founded on 22 May 1964, but which succeeded the Bank of Rhodesia and Nyasaland (1956-1963) which had been liquidated at the collapse of the Federation of Rhodesia and Nyasaland in 1963. Prior to 1956, there was a Central African Currency Board from 1953, but which had been established as the Southern Rhodesia Currency Board in 1938 to provide Rhodesian currency, fully backed and bound to the British pound sterling at par face value. The local currency which Central African Currency Board was mandated to supply to Southern Rhodesia (colonial Zimbabwe), Northern Rhodesia (colonial Zambia) and Nyasaland (colonial Malawi) had been established through the Southern Rhodesia Coinage and Currency Act of 1932. The Reserve Bank of Rhodesia (which became the Reserve Bank of Zimbabwe at independence in 1980) has con ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Zimbabwe
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rock Formations Of Africa
Rock most often refers to: * Rock (geology), a naturally occurring solid aggregate of minerals or mineraloids * Rock music, a genre of popular music Rock or Rocks may also refer to: Places United Kingdom * Rock, Caerphilly, a location in Wales * Rock, Cornwall, a village in England * Rock, County Tyrone, a village in Northern Ireland * Rock, Devon, a location in England * Rock, Neath Port Talbot, a location in Wales * Rock, Northumberland, a village in England * Rock, Somerset, a location in Wales * Rock, West Sussex, a hamlet in Washington, England * Rock, Worcestershire, a village and civil parish in England United States * Rock, Kansas, an unincorporated community * Rock, Michigan, an unincorporated community * Rock, West Virginia, an unincorporated community * Rock, Rock County, Wisconsin, a town in southern Wisconsin * Rock, Wood County, Wisconsin, a town in central Wisconsin Elsewhere * Corregidor, an island in the Philippines also known as "The Rock" * Jamaica, an isla ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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