|
Balancing Rocks Of Zimbabwe
Balancing rocks are found in many parts of Zimbabwe. These geomorphological features are formed of igneous rocks. Particularly noteworthy balancing rocks are located in Matobo 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 (at coordinates ). This 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. See also * Balancing rock * List of individual rocks The following is a list of notable rocks and stones. See also * List of largest meteorites on Earth * List of longest natural arches * List of rock formations * List of rock formations that resemble human beings * List of rocks on Mars * Lists ... References Harare Landforms of Zimbabwe Roc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Matobo 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; it 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. 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 , of which 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 Mpopoma river valleys. Part of the national park is set aside as a game park, which has been stock ... [...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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zimbabwe
file:Zimbabwe, relief map.jpg, upright=1.22, Zimbabwe, relief map Zimbabwe, officially the Republic of Zimbabwe, is a landlocked country in Southeast Africa, between the Zambezi and Limpopo Rivers, bordered by South Africa to the south, Botswana to the southwest, Zambia to the north, and Mozambique to the east. The capital and largest city is Harare, and the second largest is Bulawayo. A country of roughly 16.6 million people as per 2024 census, Zimbabwe's largest ethnic group are the Shona people, Shona, who make up 80% of the population, followed by the Northern Ndebele people, Northern Ndebele and other #Demographics, smaller minorities. Zimbabwe has 16 official languages, with English, Shona language, Shona, and Northern Ndebele language, Ndebele the most common. Zimbabwe is a member of the United Nations, the Southern African Development Community, the African Union, and the Common Market for Eastern and Southern Africa. The region was long inhabited by the San people, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Balancing Rocks
A balancing rock, also called a balanced rock, precariously balanced rock (PBR), or precarious boulder, is a naturally occurring geological formation featuring a large rock or boulder, sometimes of substantial size, resting on other rocks, bedrock, or on glacial till. Some formations known by this name only appear to be balancing, but are in fact firmly connected to a base rock by a pedestal or stem. No single scientific definition of the term exists, and it has been applied to a variety of rock features. Categories Types of feature that the term has been applied to include: ;Glacial erratic: A boulder that was transported and deposited by glaciers or ice rafts to a resting place on soil, on bedrock, or on other boulders. It usually has a different lithology from the other rocks around it. Not all glacial erratics are balancing rocks; some are firmly seated on the ground. Some balancing erratics have come to be known as rocking stones, also known as logan rocks, logan stones, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geomorphology
Geomorphology () is the scientific study of the origin and evolution of topographic and bathymetric features generated 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 comprise the action of water, wind, ice, wildfire, and lif ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Igneous
Igneous rock ( ), or magmatic rock, is one of the three main rock types, the others being sedimentary and metamorphic. Igneous rocks are 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 of the Earth's crust by volume. Igneous rocks ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Epworth, Zimbabwe
Epworth is a bedroom community in south-eastern Harare Province, Zimbabwe, located east of the city center of Harare. Its population exploded in the late 1970s and 1980s as the town saw a rise in Rural-to-urban migration, creating informal settlements. 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, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Harare
Harare ( ), formerly Salisbury, is the Capital city, capital and largest city of Zimbabwe. The city proper has an area of , a population of 1,849,600 as of the 2022 Zimbabwe census, 2022 census and an estimated 2,487,209 people in its metropolitan province. The city is situated in north-eastern Zimbabwe in the country's Mashonaland region. Harare Metropolitan Province incorporates the city and the municipalities of Chitungwiza, Epworth, Zimbabwe, Epworth and Ruwa. 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 was named Southern Rhodesia, Fort Salisbury after the British Prime Minister Robert Gascoyne-Cecil, 3rd Marquess of Salisbury, Lord Salisbury. Company Company rule in Rhodesia, administrators Demarcation line, demarcated the city and ran it until Southern Rhodesia achieved respo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zimbabwe $2 Bond Note 2016
file:Zimbabwe, relief map.jpg, upright=1.22, Zimbabwe, relief map Zimbabwe, officially the Republic of Zimbabwe, is a landlocked country in Southeast Africa, between the Zambezi and Limpopo Rivers, bordered by South Africa to the south, Botswana to the southwest, Zambia to the north, and Mozambique to the east. The capital and largest city is Harare, and the second largest is Bulawayo. A country of roughly 16.6 million people as per 2024 census, Zimbabwe's largest ethnic group are the Shona people, Shona, who make up 80% of the population, followed by the Northern Ndebele people, Northern Ndebele and other #Demographics, smaller minorities. Zimbabwe has 16 official languages, with English, Shona language, Shona, and Northern Ndebele language, Ndebele the most common. Zimbabwe is a member of the United Nations, the Southern African Development Community, the African Union, and the Common Market for Eastern and Southern Africa. The region was long inhabited by the San people, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Banknotes Of Zimbabwe
The banknotes of Zimbabwe were physical forms of Zimbabwe's first four incarnations of the Zimbabwean Dollar, dollar ($ or Z$), from 1980 to 2009. The banknotes of the first dollar replaced those of the Rhodesian dollar at par in 1981, one year after the proclamation of independence. The Reserve Bank of Zimbabwe issued most of the banknotes and other types of currency notes in its history, including the bearer cheques and special agro-cheques ("agro" being short for agricultural) that circulated between 15 September 2003 and 31 December 2008: the Standard Chartered Bank also issued their own emergency cheques from 2003 to 2004. The obverse of Zimbabwean banknotes (including Zimbabwean dollar (2019–2024)#Banknotes, notes of the Zimbabwean dollar (2019–2024), 2019-2024 dollar) featured an illustration of the Domboremari, one of the Balancing rocks of Zimbabwe, Chiremba Balancing Rocks located near Harare and Epworth, Zimbabwe, Epworth: the Domboremari also appeared on bearer ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reserve Bank Of Zimbabwe
The Reserve Bank of Zimbabwe ( RBZ) is the central bank of Zimbabwe and is headquartered in the country’s capital 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Balancing Rock
A balancing rock, also called a balanced rock, precariously balanced rock (PBR), or precarious boulder, is a naturally occurring geological formation featuring a large rock or boulder, sometimes of substantial size, resting on other rocks, bedrock, or on glacial till. Some formations known by this name only appear to be balancing, but are in fact firmly connected to a base rock by a pedestal or stem. No single scientific definition of the term exists, and it has been applied to a variety of rock features. Categories Types of feature that the term has been applied to include: ;Glacial erratic: A boulder that was transported and deposited by glaciers or ice rafts to a resting place on soil, on bedrock, or on other boulders. It usually has a different lithology from the other rocks around it. Not all glacial erratics are balancing rocks; some are firmly seated on the ground. Some balancing erratics have come to be known as rocking stones, also known as logan rocks, logan stones, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
