Balancing Rocks | |
|---|---|
Topographic feature | |
 Balancing formation seen in Matopos National Park, known as the Mother and Child inselberg | |
| Coordinates: 17°53′13.3″S31°7′51.2″E / 17.887028°S 31.130889°E | |
| Location | Zimbabwe |
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.
The Domboremari, also known as the Money Rock, [1] is a formation of three boulders that form part of the Chiremba Balancing Rocks on the northwestern outskirts of Epworth (at coordinates 17°53′08″S31°07′31″E / 17.885685°S 31.12541°E ): 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. [2] [3] [4]
Zimbabwe, officially the Republic of Zimbabwe, is a landlocked country in Southern 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.
The economy of Zimbabwe relies on the tertiary sector of the economy, also known as the service sector of the economy, which makes up to 60% of total GDP as of 2017. Zimbabwe has the second largest, by percentage, Informal economy in the world, with a score of 60.6%. Agriculture and mining largely contribute to exports. After continuous negative growth between 1999 and 2008, the economy of Zimbabwe grew 34% from 2008 to 2013, making it the fastest-growing economy in the world. Growth since then has been volatile, but averaged 5% on an end-to-end basis.
Feldspar is a group of rock-forming aluminium tectosilicate minerals, also containing other cations such as sodium, calcium, potassium, or barium. The most common members of the feldspar group are the plagioclase (sodium-calcium) feldspars and the alkali (potassium-sodium) feldspars. Feldspars make up about 60% of the Earth's crust, and 41% of the Earth's continental crust by weight.
Basalt is an aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron exposed at or very near the surface of a rocky planet or moon. More than 90% of all volcanic rock on Earth is basalt. Rapid-cooling, fine-grained basalt is chemically equivalent to slow-cooling, coarse-grained gabbro. The eruption of basalt lava is observed by geologists at about 20 volcanoes per year. Basalt is also an important rock type on other planetary bodies in the Solar System. For example, the bulk of the plains of Venus, which cover ~80% of the surface, are basaltic; the lunar maria are plains of flood-basaltic lava flows; and basalt is a common rock on the surface of Mars.
Harare, originally known as Salisbury, is the capital city of Zimbabwe.The parliamentary wing was removed from Harare upon completion of the New Parliament of Zimbabwe in April 2022, meaning that Zimbabwe has two capital cities at the moment, Mount Hampden and Harare. It is the most populous city of Zimbabwe. The city proper has an area of 981km2 (378.7 mi2) a population of 1,849,600 as of 2022 census and an estimated 2,487,209 in its metropolitan province according to 2022 Census as well. 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 1,483 metres above sea level, and its climate falls into the subtropical highland category.
In geology, rock is any naturally occurring solid mass or aggregate of minerals or mineraloid matter. It is categorized by the minerals included, its chemical composition, and the way in which it is formed. Rocks form the Earth's outer solid layer, the crust, and most of its interior, except for the liquid outer core and pockets of magma in the asthenosphere. The study of rocks involves multiple subdisciplines of geology, including petrology and mineralogy. It may be limited to rocks found on Earth, or it may include planetary geology that studies the rocks of other celestial objects.
Metamorphism is the transformation of existing rock to rock with a different mineral composition or texture. Metamorphism takes place at temperatures in excess of 150 °C (300 °F), and often also at elevated pressure or in the presence of chemically active fluids, but the rock remains mostly solid during the transformation. Metamorphism is distinct from weathering or diagenesis, which are changes that take place at or just beneath Earth's surface.
Garden of the Gods is a 1,341.3 acre public park located in Colorado Springs, Colorado, United States. 862 acres of the park was designated a National Natural Landmark in 1971.
The Vredefort impact structure is one of the largest verified impact structures on Earth. The crater, which has since been eroded away, has been estimated at 170 kilometres (110 mi) to 300 km (190 mi) across when it was formed. The remaining structure, comprising the deformed underlying bedrock, is located in present-day Free State province of South Africa. It is named after the town of Vredefort, which is near its centre. The structure's central uplift is known as the Vredefort Dome. The impact structure was formed during the Paleoproterozoic Era, 2.023 billion years ago. It is the second-oldest known impact structure on Earth, after Yarrabubba.
The Zimbabwe National Army (ZNA) is the primary branch of the Zimbabwe Defence Forces responsible for land-oriented military operations. It is the largest service branch under the Zimbabwean Joint Operations Command (JOC). The modern army has its roots in the Rhodesian Army, which was raised between 1963 and 1964 after the breakup of the Federation of Rhodesia and Nyasaland. A ''Joint High Command created in March 1980 to oversee integration of the formerly belligerent Rhodesian Security Forces, Zimbabwe African National Liberation Army (ZANLA), and the Zimbabwe People's Revolutionary Army (ZIPRA) officially established the Zimbabwe National Army in late 1980, nearly a year after the end of the Rhodesian Bush War.
The Reserve Bank of Zimbabwe is the central bank of Zimbabwe and is headquartered in the capital city Harare.
The Karoo Supergroup is the most widespread stratigraphic unit in Africa south of the Kalahari Desert. The supergroup consists of a sequence of units, mostly of nonmarine origin, deposited between the Late Carboniferous and Early Jurassic, a period of about 120 million years.
The Pan-African orogeny was a series of major Neoproterozoic orogenic events which related to the formation of the supercontinents Gondwana and Pannotia about 600 million years ago. This orogeny is also known as the Pan-Gondwanan or Saldanian Orogeny. The Pan-African orogeny and the Grenville orogeny are the largest known systems of orogenies on Earth. The sum of the continental crust formed in the Pan-African orogeny and the Grenville orogeny makes the Neoproterozoic the period of Earth's history that has produced most continental crust.
Type locality, also called type area, is the locality where a particular rock type, stratigraphic unit or mineral species is first identified. If the stratigraphic unit in a locality is layered, it is called a stratotype, whereas the standard of reference for unlayered rocks is the type locality.
Hyperinflation in Zimbabwe is an ongoing period of currency instability in Zimbabwe which, using Cagan's definition of hyperinflation, began in February 2007. During the height of inflation from 2008 to 2009, it was difficult to measure Zimbabwe's hyperinflation because the government of Zimbabwe stopped filing official inflation statistics. However, Zimbabwe's peak month of inflation is estimated at 79.6 billion percent month-on-month, 89.7 sextillion percent year-on-year in mid-November 2008.
The banknotes of Zimbabwe were physical forms of Zimbabwe's first four incarnations of the dollar, 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 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 Zimbabwean dollar was the name of four official currencies of Zimbabwe from 1980 to 12 April 2009. During this time, it was subject to periods of extreme inflation, followed by a period of hyperinflation.
A balancing rock, also called a balanced rock 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.
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