Anyolite (corundum-amphibole Zoisitite) (Neoproterozoic; Mundarara Mine, About 27 Km West Of Longido
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Anyolite (corundum-amphibole Zoisitite) (Neoproterozoic; Mundarara Mine, About 27 Km West Of Longido
Anyolite is a metamorphic rock composed of intergrown green zoisite, black/dark green pargasite and ruby.http://www.mindat.org/min-27151.html Mindat It has been found in the Arusha Region of Tanzania and in Austria. It is sometimes incorrectly advertised as a variety of the mineral zoisite. The term ''anyolite'' is, however, not an officially accepted term for a metamorphic rock. Its name derives from the Maasai word ''anyoli'', meaning "green". Anyolite is also referred to as ruby in zoisite, ruby zoisite, ruby-zoisite or Tanganyika artstone. The contrasting colours make anyolite a popular material for sculptures and other decorative objects. It was first discovered at the Mundarara Mine, near Longido, Tanzania in 1954. In 2010 it was suggested that a 2 kilogram stone known as the ''Gem of Tanzania'' owned by the defunct company Wrekin Construction and fraudulently valued at £11 million was actually a lump of anyolite worth about £100, although it was eventually sold for ...
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Anyolite (corundum-amphibole Zoisitite) (Neoproterozoic; Mundarara Mine, About 27 Km West Of Longido, Tanzania) 2 (49144140952)
Anyolite is a metamorphic rock composed of intergrown green zoisite, black/dark green pargasite and ruby.http://www.mindat.org/min-27151.html Mindat It has been found in the Arusha Region of Tanzania and in Austria. It is sometimes incorrectly advertised as a variety of the mineral zoisite. The term ''anyolite'' is, however, not an officially accepted term for a metamorphic rock. Its name derives from the Maasai language, Maasai word ''anyoli'', meaning "green". Anyolite is also referred to as ruby in zoisite, ruby zoisite, ruby-zoisite or Tanganyika artstone. The contrasting colours make anyolite a popular material for sculptures and other decorative objects. It was first discovered at the Mundarara Mine, near Longido, Tanzania in 1954. In 2010 it was suggested that a 2 kilogram stone known as the ''Gem of Tanzania'' owned by the defunct company Wrekin Construction and fraudulently valued at £11 million was actually a lump of anyolite worth about £100, although it was eventual ...
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Metamorphic Rock
Metamorphic rocks arise from the transformation of existing rock to new types of rock in a process called metamorphism. The original rock ( protolith) is subjected to temperatures greater than and, often, elevated pressure of or more, causing profound physical or chemical changes. During this process, the rock remains mostly in the solid state, but gradually recrystallizes to a new texture or mineral composition. The protolith may be an igneous, sedimentary, or existing metamorphic rock. Metamorphic rocks make up a large part of the Earth's crust and form 12% of the Earth's land surface. They are classified by their protolith, their chemical and mineral makeup, and their texture. They may be formed simply by being deeply buried beneath the Earth's surface, where they are subject to high temperatures and the great pressure of the rock layers above. They can also form from tectonic processes such as continental collisions, which cause horizontal pressure, friction, and dist ...
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Zoisite
Zoisite, first known as saualpite, after its type locality, is a calcium aluminum hydroxy sorosilicate belonging to the epidote group of minerals. Its chemical formula is Ca2 Al3( Si O4)(Si2O7)O(O H). Zoisite occurs as prismatic, orthorhombic (2/m 2/m 2/m) crystals or in massive form, being found in metamorphic and pegmatitic rock. Zoisite may be blue to violet, green, brown, pink, yellow, gray, or colorless. Blue crystals are known under the name tanzanite. It has a vitreous luster and a conchoidal to uneven fracture. When euhedral, zoisite crystals are striated parallel to the principal axis (c-axis). Also parallel to the principal axis is one direction of perfect cleavage. The mineral is between 6 and 7 on the Mohs hardness scale, and its specific gravity ranges from 3.10 to 3.38, depending on the variety. It streaks white and is said to be brittle. Clinozoisite is a more common monoclinic polymorph of Ca2Al3(SiO4)(Si2O7)O(OH). Transparent material is fashioned ...
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Pargasite
Pargasite or ''pargasitic hornblende'' is a complex Silicate mineral, inosilicate mineral of the amphibole group with formula NaCa2(Mg4Al)(Si6Al2)O22(OH)2. It was first described for an occurrence in Pargas, Finland in 1814 and named for the locality. It occurs in high temperature regional metamorphic rocks and in the skarns within contact metamorphism, contact aureoles around igneous intrusions. It also occurs in andesite volcanic rocks and altered ultramafic rocks. Pargasite is the main water-storage site in the uppermost Mantle (geology), mantle; however, it becomes unstable at depths greater than . This has significant consequences for the water storage capacity, and the solidus temperature of the lherzolite of the upper mantle (Earth), upper mantle. It is used as a gemstone. See also *Anyolite References
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Ruby
Ruby is a pinkish-red-to-blood-red-colored gemstone, a variety of the mineral corundum ( aluminium oxide). Ruby is one of the most popular traditional jewelry gems and is very durable. Other varieties of gem-quality corundum are called sapphires; given that the rest of the corundum species are called as such, rubies are sometimes referred to as "red sapphires". Ruby is one of the traditional cardinal gems, alongside amethyst, sapphire, emerald, and diamond. The word ''ruby'' comes from ''ruber'', Latin for red. The color of a ruby is due to the presence of chromium. Some gemstones that are popularly or historically called rubies, such as the Black Prince's Ruby in the British Imperial State Crown, are actually spinels. These were once known as "Balas rubies". The quality of a ruby is determined by its color, cut, and clarity, which, along with carat weight, affect its value. The brightest and most valuable shade of red, called blood-red or pigeon blood, commands a lar ...
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Arusha Region
Arusha Region () is one of Tanzania's 31 administrative Regions of Tanzania, regions and is located in the northeast of the country. The region's capital and largest city is the city of Arusha. The region is bordered by Kajiado County and Narok County in Kenya to the north, the Kilimanjaro Region to the east, the Manyara Region, Manyara and Singida Region, Singida Regions to the south, and the Mara Region, Mara and Simiyu Region, Simiyu regions to the west. Arusha Region is home to Ngorongoro Conservation Area, a UNESCO World Heritage Site. The region is comparable in size to the combined land and water areas of the state of Maryland in the United States. Arusha Region is a tourist destination in Africa and is the hub of the northern Tanzania safari circuit. The national parks and nature reserves in this region include Ngorongoro Conservation Area, Arusha National Park, the Loliondo Game Controlled Area, and part of Lake Manyara National Park. Remains of 600-year-old stone structu ...
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Tanzania
Tanzania, officially the United Republic of Tanzania, is a country in East Africa within the African Great Lakes region. It is bordered by Uganda to the northwest; Kenya to the northeast; the Indian Ocean to the east; Mozambique and Malawi to the south; Zambia to the southwest; and Rwanda, Burundi, and the Democratic Republic of the Congo to the west. According to a 2024 estimate, Tanzania has a population of around 67.5 million, making it the most populous country located entirely south of the equator. Many important hominid fossils have been found in Tanzania. In the Stone and Bronze Age, prehistoric migrations into Tanzania included South Cushitic languages, Southern Cushitic speakers similar to modern day Iraqw people who moved south from present-day Ethiopia; Eastern Cushitic people who moved into Tanzania from north of Lake Turkana about 2,000 and 4,000 years ago; and the Southern Nilotic languages, Southern Nilotes, including the Datooga people, Datoog, who originated fro ...
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Mineral
In geology and mineralogy, a mineral or mineral species is, broadly speaking, a solid substance with a fairly well-defined chemical composition and a specific crystal structure that occurs naturally in pure form.John P. Rafferty, ed. (2011): Minerals'; p. 1. In the series ''Geology: Landforms, Minerals, and Rocks''. Rosen Publishing Group. The Geology, geological definition of mineral normally excludes compounds that occur only in living organisms. However, some minerals are often biogenic (such as calcite) or organic compounds in the sense of chemistry (such as mellite). Moreover, living organisms often synthesize inorganic minerals (such as hydroxylapatite) that also occur in rocks. The concept of mineral is distinct from rock (geology), rock, which is any bulk solid geologic material that is relatively homogeneous at a large enough scale. A rock may consist of one type of mineral or may be an aggregate (geology), aggregate of two or more different types of minerals, spaci ...
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Maasai Language
Maasai (previously spelled ''Masai'') or Maa ( ; autonym: ''ɔl Maa'') is an Eastern Nilotic language spoken in Southern Kenya and Northern Tanzania by the Maasai people, numbering about 1.5 million. It is closely related to the other Maa varieties: Samburu (or Sampur), the language of the Samburu people of central Kenya, Chamus, spoken south and southeast of Lake Baringo (sometimes regarded as a dialect of Samburu); and Parakuyu of Tanzania. The Maasai, Samburu, il-Chamus and Parakuyu peoples are historically related and all refer to their language as . Properly speaking, "Maa" refers to the language and the culture and "Maasai" refers to the people "who speak Maa". Phonology The Maasai variety of as spoken in southern Kenya and Tanzania has 30 contrasting phonemes, including a series of implosive consonants. In Maasai, tone has a very productive role, conveying a wide range of grammatical and semantic functions. Consonants In the table of consonant phonemes bel ...
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Mundarara Mine
} Mundarara is an administrative ward in the Longido District of the Arusha Region of Tanzania. The ward covers an area of , and has an average elevation of . According to the 2012 census, the ward has a total population of 7,301. the mineral Anyolite Anyolite is a metamorphic rock composed of intergrown green zoisite, black/dark green pargasite and ruby.http://www.mindat.org/min-27151.html Mindat It has been found in the Arusha Region of Tanzania and in Austria. It is sometimes incorrectly adv ... was first discovered there. References Wards of Longido Wards of Arusha Region {{Arusha-geo-stub ...
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Longido
Longido or Longido Town (''Kata na Mji wa Lingido'' in Swahili) is an administrative ward and district capital located in the Longido District of the Arusha Region of Tanzania. The ward is bordered to the south on three sides by Orbomba ward and to the north by Kimokouwa ward. It is the administrative seat for Longido District. According to the 2012 census, the ward has a total population of 2,241. Longido is at the foot of Mount Longido. History On 3 November 1914, German forces defeated a British Expeditionary Force near Longido at the Battle of Kilimanjaro. A 1928 ascent of Mount Longido was described in Vivienne de Watteville's book ''Speak to the Earth'' (1935). Anyolite was first discovered at the Mundarara Mine near Longido in 1954.In 2007, Longido became the capital of Longido District, which was formed out of part of Monduli District 'Monduli District (''Wilaya ya Monduli'', in Swahili language, Swahili) is one of seven Districts of Tanzania, districts of the Aru ...
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Wrekin Construction
The Wrekin ( ) is a hill in east Shropshire, England. It is located some west of Telford, on the border between the unitary authorities of Shropshire and Telford and Wrekin. Rising above the Shropshire Plain to a height of above sea level, it is a prominent and well-known landmark, signalling the entrance to Shropshire for travellers westbound on the M54 motorway. The Wrekin is contained within the northern salient of the Shropshire Hills AONB. The hill is popular with walkers and tourists and offers good views of Shropshire. It can be seen well into Staffordshire and the Black Country, and even as far as the Beetham Tower in Manchester, Winter Hill in Lancashire and Cleeve Hill in Gloucestershire. Name The earliest mention of ''the Wrekin'' occurs in a charter of 855, as entered in a late 11th-century Worcester cartulary, spelled ''Wreocensetun''. Its modern form is believed to have come into modern English by way of Mercian, and that is likely to have been taken from th ...
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