quinta-feira, 4 de agosto de 2016

The Mohs scale of mineral hardness is a qualitative ordinal scale that characterizes

The Mohs scale of mineral hardness is a qualitative ordinal scale that characterizes the scratch resistance of various minerals through the ability of a harder material to scratch a softer material. It was created in 1812 by the German geologist and mineralogist Friedrich Mohs and is one of several definitions of hardness in materials science, some of which are more quantitative.

The method of comparing hardness by seeing which minerals can visibly scratch others, however, is of great antiquity, having been mentioned by Theophrastus in his treatise On Stones, c. 300 BC, followed by Pliny the Elder in his Naturalis Historia, c. 77 AD. While greatly facilitating the identification of minerals in the field, the Mohs scale does not show how well hard materials perform in an industrial setting.

About Hardness Tests

The hardness test developed by Friedrich Mohs was the first known test to assess resistance of a material to scratching. It is a very simple but inexact comparative test. Perhaps its simplicity has enabled it to become the most widely used hardness test.

Since the Mohs Scale was developed in 1812, many different hardness tests have been invented. These include tests by Brinell, Knoop, Rockwell, Shore and Vickers. Each of these tests uses a tiny "indenter" that is applied to the material being tested with a carefully measured amount of force. Then the size or the depth of the indentation and the amount of force are used to calculate a hardness value.

Because each of these tests uses a different apparatus and different calculations they can not be directly compared to one another. So if the Knoop hardness test was done the number is usually reported as a "Knoop hardness". For this reason, Mohs hardness test results should also be reported as a "Mohs hardness."

Why are there so many different hardness tests? The type of test used is determined by the size, shape and other characteristics of the specimens being tested. Although these tests are quite different from the Mohs test there is some correlation between them.

Usage

Despite its simplicity and lack of precision, the Mohs scale is highly relevant for field geologists, who use the scale to roughly identify minerals using scratch kits. The Mohs scale hardness of minerals can be commonly found in reference sheets. Reference materials may be expected to have a uniform Mohs hardness.

Minerals

The Mohs scale of mineral hardness is based on the ability of one natural sample of mineral to scratch another mineral visibly. The samples of matter used by Mohs are all different minerals. Minerals are pure substances found in nature. Rocks are made up of one or more minerals.

As the hardest known naturally occurring substance when the scale was designed, diamonds are at the top of the scale. The hardness of a material is measured against the scale by finding the hardest material that the given material can scratch, and/or the softest material that can scratch the given material. For example, if some material is scratched by apatite but not by fluorite, its hardness on the Mohs scale would fall between 4 and 5.

"Scratching" a material for the purposes of the Mohs scale means creating non-elastic dislocations visible to the naked eye. Frequently, materials that are lower on the Mohs scale can create microscopic, non-elastic dislocations on materials that have a higher Mohs number. While these microscopic dislocations are permanent and sometimes detrimental to the harder material's structural integrity, they are not considered "scratches" for the determination of a Mohs scale number.

The Mohs scale is a purely ordinal scale. For example, corundum (9) is twice as hard as topaz (8), but diamond (10) is four times as hard as corundum. The table below shows the comparison with the absolute hardness measured by a sclerometer, with pictorial examples.

Mohs Hardness Scale  

Mohs Hardness Scale
Mineral
Hardness
Talc
1
Gypsum
2
Calcite
3
Fluorite
4
Apatite
5
Orthoclase
6
Quartz
7
Topaz
8
Corundum
9
Diamond
10

Mohs Hardness of Common Minerals

Alphabetical
Mineral
Mohs Hardness
Anhydrite3 to 3.5
Apatite5
Arsenopyrite5.5 to 6
Augite5.5 to 6
Azurite3.5 to 4
Barite2.5 to 3.5
Bauxite1 to 3
Beryl7.5 to 8
Biotite2.5 to 3
Bornite3 to 3.25
Calcite3
Cassiterite6 to 7
Chalcocite2.5 to 3
Chalcopyrite3.5 to 4
Chlorite2 to 2.5
Chromite5.5 to 6
Chrysoberyl8.5
Cinnabar2 to 2.5
Copper2.5 to 3
Cordierite7 to 7.5
Corundum9
Cuprite3.5 to 4
Diamond10
Diopside5.5 to 6.5
Dolomite3.5 to 4
Enstatite5 to 6
Epidote6 to 7
Fluorite4
Galena2.5 to 2.75
Garnet6.5 to 7.5
Glauconite2
Gold2.5 to 3
Graphite1 to 2
Gypsum1.5 to 2
Halite2 to 2.5
Hematite5 to 6.5
Hornblende5 to 6
Ilmenite5 to 6
Jadeite6.5 to 7
Kyanite4.5 to 5 or 7
Limonite1 to 5
Magnesite3.5 to 5
Magnetite5 to 6.5
Malachite3.5 to 4
Marcasite6 to 7.5
Molybdenite1 to 2
Monazite5 to 5.5
Muscovite2 to 3
Nepheline5.5 to 6
Nephrite5 to 6
Olivine6.5 to 7
Orthoclase6 to 6.5
Plagioclase6 to 6.5
Prehnite6 to 6.5
Pyrite6 to 6.5
Pyrophyllite1 to 2
Pyrrhotite3.5 to 4.5
Quartz7
Rhodochrosite3.5 to 4
Rhodonite5.5 to 6.5
Rutile6 to 6.5
Serpentine3 to 5
Siderite3.5 to 4.5
Sillimanite6.5 to 7.5
Silver2.5 to 3
Sodalite5.5 to 6
Sphalerite3.5 to 4
Spinel7.5 to 8
Spodumene6.5 to 7
Staurolite7 to 7.5
Sulfur1.5 to 2.5
Sylvite2
Talc1
Titanite5 to 5.5
Topaz8
Tourmaline7 to 7.5
Turquoise5 to 6
Uraninite5 to 6
Witherite3 to 3.5
Wollastonite4.5 to 5.5
Zircon7.5
Zoisite6 to 7
Decreasing Hardness
Mineral
Mohs Hardness
Diamond10
Corundum9
Chrysoberyl8.5
Topaz8
Beryl7.5 to 8
Spinel7.5 to 8
Zircon7.5
Cordierite7 to 7.5
Staurolite7 to 7.5
Tourmaline7 to 7.5
Quartz7
Garnet6.5 to 7.5
Jadeite6.5 to 7
Sillimanite6.5 to 7.5
Olivine6.5 to 7
Spodumene6.5 to 7
Marcasite6 to 7.5
Cassiterite6 to 7
Epidote6 to 7
Zoisite6 to 7
Orthoclase6 to 6.5
Plagioclase6 to 6.5
Prehnite6 to 6.5
Pyrite6 to 6.5
Rutile6 to 6.5
Diopside5.5 to 6.5
Rhodonite5.5 to 6.5
Arsenopyrite5.5 to 6
Augite5.5 to 6
Chromite5.5 to 6
Hematite5.5 to 6.5
Nepheline5.5 to 6
Sodalite5.5 to 6
Magnetite5 to 6.5
Enstatite5 to 6
Hornblende5 to 6
Ilmenite5 to 6
Nephrite5 to 6
Turquoise5 to 6
Uraninite5 to 6
Monazite5 to 5.5
Titanite5 to 5.5
Apatite5
Wollastonite4.5 to 5.5
Kyanite4.5 to 5 or 7
Fluorite4
Magnesite3.5 to 5
Pyrrhotite3.5 to 4.5
Siderite3.5 to 4.5
Azurite3.5 to 4
Chalcopyrite3.5 to 4
Cuprite3.5 to 4
Dolomite3.5 to 4
Malachite3.5 to 4
Rhodochrosite3.5 to 4
Sphalerite3.5 to 4
Serpentine3 to 5
Anhydrite3 to 3.5
Witherite3 to 3.5
Bornite3 to 3.25
Calcite3
Barite2.5 to 3.5
Biotite2.5 to 3
Chalcocite2.5 to 3
Copper2.5 to 3
Gold2.5 to 3
Silver2.5 to 3
Galena2.5 to 2.75
Muscovite2 to 3
Chlorite2 to 2.5
Cinnabar2 to 2.5
Halite2 to 2.5
Glauconite2
Sylvite2
Sulfur1.5 to 2.5
Gypsum1.5 to 2
Limonite1 to 5
Bauxite1 to 3
Graphite1 to 2
Molybdenite1 to 2
Pyrophyllite1 to 2
Talc1

Mohs Hardness of Common Objects
Fingernail2 to 2.5
Copper3
Nail4
Glass5.5
Knife blade5 to 6.5
Steel file6.5
Streak plate6.5 to 7
Quartz7



TOP 10 WORLD'S RAREST GEMS


A gemstone or gem (also called a fine gem, jewel, or a precious or semi-precious stone) is a piece of mineral crystal, which, in cut and polished form, is used to make jewelry or other adornments.

However, certain rocks (such as lapis lazuli) or organic materials that are not minerals (such as amber or jet), are also used for jewelry, and are therefore often considered to be gemstones as well. Most gemstones are hard, but some soft minerals are used in jewelry because of their luster or other physical properties that have aesthetic value. Rarity is another characteristic that lends value to a gemstone. Apart from jewelry, from earliest antiquity engraved gems and hardstone carvings, such as cups, were major luxury art forms. A gem maker is called a lapidary or gemcutter; a diamond worker is a diamantaire.

Throughout history, humans have adorned themselves with jewelry - first made from bits of shell, bone and sparkly rocks, and later, with gems set in copper, silver and gold.

It takes millions of years for crystals to form in nature, and only a fraction of those will ever be found, mined, cut and sold as gemstones. The value of gemstones depends on many factors, including rarity, quality, setting, and even politics. Dig in to the world of incredibly expensive jewels with our rundown of ten of the world's rarest and most valuable gemstones.

1. Tanzanite

Sun Chan/Getty Images
Tanzanite is the blue/violet variety of the mineral zoisite (a calcium aluminium hydroxyl Sorosilicate) belonging to the epidote group. It was discovered in the Mererani Hills of Manyara Region in Northern Tanzania in 1967, near the city of Arusha and Mount Kilimanjaro. Tanzanite is used as a relatively cheap gemstone, where it can substitute for the far more expensive sapphire after undergoing artificial heat treatment to form a deep blue coloration. Naturally formed tanzanite is extremely rare and is endemic only to the Mererani Hills.

The mineral was named by Tiffany & Co. after Tanzania, the country in which it was discovered. In 2002, the American Gem Trade Association chose Tanzanite as a December birthstone, the first change to their birthstone list since 1912

Composition: Calcium, Aluminum, Silicon, Hydrogen, Oxygen | Market Value: $600-$1,000 per carat. 

2. Taaffeite
Richard Leeney/Getty Images

Taaffeite is a mineral, named after its discoverer Richard Taaffe (1898–1967) who found the first sample, a cut and polished gem, in October 1945 in a jeweler's shop in Dublin, Ireland. As such, it is the only gemstone to have been initially identified from a faceted stone. Most pieces of the gem, prior to Taaffe, had been misidentified as spinel. For many years afterwards, it was known only in a few samples, and is still one of the rarest gemstone minerals in the world.

Since 2002, the International Mineralogical Association-approved name for taaffeite as a mineral is magnesiotaaffeite-2N'2S.

Discovery

Taaffe bought a number of precious stones from a jeweller in October 1945. Upon noticing inconsistencies between the taaffeite and spinels, Taaffe sent some examples to B. W. Anderson of the Laboratory of the London Chamber of Commerce for identification on 1 November 1945. When Anderson replied on 5 November 1945, he told Taaffe that they were unsure of whether it was a spinel or something new; he also offered to write it up in Gemologist.

Composition: Magnesium, Beryllium, Aluminum, Oxygen | Market Value: $1500-$2500 per carat.

3. Black opal

Cut and polished black opal from Lightning Ridge, Australia, 16.42 carats.
Credit: Daniel Mekis/Wikipedia
Opal is a hydrated amorphous form of silica (SiO2·nH2O); its water content may range from 3 to 21% by weight, but is usually between 6 and 10%. Because of its amorphous character, it is classed as a mineraloid, unlike crystalline forms of silica, which are classed as minerals. It is deposited at a relatively low temperature and may occur in the fissures of almost any kind of rock, being most commonly found with limonite, sandstone, rhyolite, marl, and basalt. Opal is the national gemstone of Australia.

The internal structure of precious opal makes it diffract light; depending on the conditions in which it formed, it can take on many colors. Precious opal ranges from clear through white, gray, red, orange, yellow, green, blue, magenta, rose, pink, slate, olive, brown, and black. Of these hues, the black opals are the most rare, whereas white and greens are the most common. It varies in optical density from opaque to semitransparent.

Black Opal is a greenish type of opal with black mottling and gold flecks. Usually found in ancient hot springs, the gem is usually tumbled smooth and cut cabochon. The phrase in the North "Black as a black opal" means, effectively, not very black (or evil) at all, and is used to describe good-hearted rogues and similar individuals who would be embarrassed by praise. A typical specimen has a base value of 1000gp.

Composition: Silicon, Hydrogen, Oxygen | Market Value: $2,355 per carat.

4. Benitoite

Benitoite crystals under UV light
Credit: Parent Géry/Wikipedia
Benitoite is a rare blue barium titanium silicate mineral, found in hydrothermally altered serpentinite. Benitoite fluoresces under short wave ultraviolet light, appearing bright blue to bluish white in color. The more rarely seen clear to white benitoite crystals fluoresce red under long-wave UV light.

It was first described in 1907 by George D. Louderback, who named it benitoite for its occurrence near the headwaters of the San Benito River in San Benito County, California.

Benitoite occurs in a number of sites, but gemstone quality material has only been found in California. In 1985 benitoite was named as the official state gem of California.

Benitiote has a rare 5 pointed crystal form, and an even rarer 6 pointed form, "star of David", with about 24 samples known.

Composition: Barium, Titanium, Silicon, Oxygen | Market Value: $3000-$4000 per carat.

5. Red beryl

Beryl (Var: Red Beryl)
Locality: Ruby Violet claims (Violet mine; Red Emerald mine;
Harris mine), Wah Wah Mts, Beaver Co., Utah, USA
Credit: Jason B. Smith
In geology, beryl is a mineral composed of beryllium aluminium cyclosilicate with the chemical formula Be3Al2(Si O3)6. The hexagonal crystals of beryl may be very small or range to several meters in size. Terminated crystals are relatively rare. Pure beryl is colorless, but it is frequently tinted by impurities; possible colors are green, blue, yellow, red, and white.

Red beryl (formerly known as "bixbite" and marketed as "red emerald" or "scarlet emerald") is a red variety of beryl. It was first described in 1904 for an occurrence, its type locality, at Maynard's Claim (Pismire Knolls), Thomas Range, Juab County, Utah. The old synonym "bixbite" is deprecated from the CIBJO, because of the risk of confusion with the mineral bixbyite (also named after the mineralogist Maynard Bixby). The dark red color is attributed to Mn3+ ions.

Red beryl is very rare and has been reported only from a handful of locations including: Wah Wah Mountains, Beaver County, Utah; Paramount Canyon and Round Mountain, Sierra County, New Mexico, although the latter locality does not often produce gem grade stones; and Juab County, Utah. The greatest concentration of gem-grade red beryl comes from the Ruby-Violet Claim in the Wah Wah Mountains of the Thomas range of mid-western Utah, discovered in 1958 by Lamar Hodges, of Fillmore, Utah, while he was prospecting for uranium. Red beryl has been known to be confused with pezzottaite, a caesium analog of beryl, that has been found in Madagascar and more recently Afghanistan; cut gems of the two varieties can be distinguished from their difference in refractive index, and rough crystals can be easily distinguished by differing crystal systems (pezzottaite trigonal, red beryl hexagonal). Synthetic red beryl is also produced.

While gem beryls are ordinarily found in pegmatites and certain metamorphic stones, red beryl occurs in topaz-bearing rhyolites. It is formed by crystallizing under low pressure and high temperature from a pneumatolytic phase along fractures or within near-surface miarolitic cavities of the rhyolite. Associated minerals include bixbyite, quartz, orthoclase, topaz, spessartine, pseudobrookite and hematite.

Composition: Beryllium, Aluminum, Silicon, Oxygen | Market Value: $10,000 per carat.

6. Alexandrite

Alexandrite Cushion, 26.75 cts. Bluish green in daylight and purple
red under incandescent light, alexandrites this large are extremely rare.
Credit: David Weinberg/Wikipedia
The alexandrite variety displays a color change (alexandrite effect) dependent upon the nature of ambient lighting. Alexandrite effect is the phenomenon of an observed color change from greenish to reddish with a change in source illumination. Alexandrite results from small scale replacement of aluminium by chromium ions in the crystal structure, which causes intense absorption of light over a narrow range of wavelengths in the yellow region (580 nm) of the visible light spectrum. Because human vision is more sensitive to light in the green spectrum and the red spectrum, alexandrite appears greenish in daylight where a full spectrum of visible light is present and reddish in incandescent light which emits less green and blue spectrum. This color change is independent of any change of hue with viewing direction through the crystal that would arise from pleochroism.

Alexandrite from the Ural Mountains in Russia can be green by daylight and red by incandescent light. Other varieties of alexandrite may be yellowish or pink in daylight and a columbine or raspberry red by incandescent light.

Stones that show a dramatic color change and strong colors (e.g. red-to-green) are rare and sought-after, but stones that show less distinct colors (e.g. yellowish green changing to brownish yellow) may also be considered alexandrite by gem labs such as the Gemological Institute of America.

According to a popular but controversial story, alexandrite was discovered by the Finnish mineralogist Nils Gustaf Nordenskiöld (1792–1866), and named alexandrite in honor of the future Tsar Alexander II of Russia. Nordenskiöld's initial discovery occurred as a result of an examination of a newly found mineral sample he had received from Perovskii, which he identified as emerald at first. The first emerald mine had been opened in 1831.

Alexandrite 5 carats (1,000 mg) and larger were traditionally thought to be found only in the Ural Mountains, but have since been found in larger sizes in Brazil. Other deposits are located in India (Andhra Pradesh), Madagascar, Tanzania and Sri Lanka. Alexandrite in sizes over three carats are very rare.

Composition: Beryllium, Aluminum, Oxygen | Market Value: $12,000 per carat.

7. Jadeite

Jadeite from Burma
Credit: Dave Dyet/Wikipedia
Jadeite is a pyroxene mineral with composition NaAlSi2O6. It is monoclinic. It has a Mohs hardness of about 6.5 to 7.0 depending on the composition. The mineral is dense, with a specific gravity of about 3.4. Jadeite forms solid solutions with other pyroxene endmembers such as augite and diopside (CaMg-rich endmembers), aegirine (NaFe endmember), and kosmochlor (NaCr endmember). Pyroxenes rich in both the jadeite and augite endmembers are known as omphacite.

The name jadeite is derived from the Spanish phrase "piedra de ijada" which means "stone of the side". It was believed to cure kidney stones if it was rubbed against the side of the afflicted person's body. The Latin version of the name, lapis nephriticus, is the origin of the term nephrite, which is also a variety of jade.

Jadeite is formed in metamorphic rocks under high pressure and relatively low temperature conditions. Albite (NaAlSi3O8) is a common mineral of the Earth's crust, and it has a specific gravity of about 2.6, much less than that of jadeite. With increasing pressure, albite breaks down to form the high-pressure assemblage of jadeite plus quartz. Minerals associated with jadeite include: glaucophane, lawsonite, muscovite, aragonite, serpentine and quartz.

Composition: Sodium, Aluminum, Iron, Silicon, Oxygen | Market Value: $20,000 per carat./b

8. Musgravite


This 0.86 ct gray musgravite displays an unusual iridescent phenomenon that is clearly visible in the table facet.
Credit: Kevin Schumacher.
Musgravite, Be(Mg, Fe, Zn)2Al6O12, is a gemstone reportedly named after the Musgrave Ranges, Australia, where it was first discovered. It is a synonym of magnesiotaaffeite-6N’3SIt, a member of the taaffeite family of minerals. Its hardness is 8 to 8.5 on the Mohs scale.

Composition: Magnesium, Beryllium, Aluminum, Zinc, Iron, Oxygen | Market Value: $35,000 per carat.

9. Painite

Painite from Myanmar. Specimen size 2 cm long
Credit: Strickja/Wikipedia
Painite is a very rare borate mineral. It was first found in Myanmar by British mineralogist and gem dealer Arthur C.D. Pain in the 1950s. When it was confirmed as a new mineral species, the mineral was named after him.

The chemical makeup of painite contains calcium, zirconium, boron, aluminium and oxygen (CaZrAl9O15(BO3)). The mineral also contains trace amounts of chromium and vanadium. Painite has an orange-red to brownish-red color similar to topaz due to trace amounts of iron. The crystals are naturally hexagonal in shape, and, until late 2004, only two had been cut into faceted gemstones.

Composition: Calcium, Zirconium, Boron, Aluminum, Oxygen | Market Value: $50,000-$60,000 per carat.

10. Pink Star Diamond

Credit: TYRONE SIU/Reuters/Corbis
The Pink Star, formerly known as the Steinmetz Pink, is a diamond weighing 59.60 carat (11.92 g), rated in color as Fancy Vivid Pink by the Gemological Institute of America. The Pink Star was mined by De Beers in 1999 in South Africa, and weighed 132.5 carat in the rough. The Pink Star is the largest known diamond having been rated Vivid Pink. As a result of this exceptional rarity, the Steinmetz Group took a cautious 20 months to cut the Pink. It was unveiled in Monaco on 29 May 2003 in a public ceremony.

The Pink Star was displayed (as the Steinmetz Pink) as part of the Smithsonian's "The Splendor of Diamonds" exhibit, alongside the De Beers Millennium Star, the world’s second largest (the Centenary Diamond is the largest) top colour (D) internally and externally flawless pear-shaped diamond at 203.04 carat (40.608 g), the Heart of Eternity Diamond, a 27.64 carat (5.582 g) heart-cut blue diamond and the Moussaieff Red Diamond, the world's largest known Fancy Red diamond at 5.11 carat (1.022 g).

Composition: Carbon | Market Value: $83,187,381, or about $1,395,761 per carat


ESMERALDA

ESMERALDA

Esmeralda é uma das 4 pedras preciosas e uma das pedras mais populares na joalheria. É parte da família do Berilo. Sua cor verde vem do vanádio e cromo, o verde é mais intenso e de grande qualidade. Sua dureza é de 7,5-8 na escala de Mohs, que é conveniente, mas exige aos joalheiros muita atenção na hora de criar uma peça, pois sua constituição é frágil e quebradiça.

A esmeralda tem, efetivamente, inclusões chamadas "jardins" ou "gelo" é dito que a esmeralda é habitada. Os jardins são realmente cheios de cristais ou bolhas de gás, às vezes líquidos. são destes cristais que caracterizam uma esmeralda. O mais puro tem poucas inclusões, mas isso é raro e aumenta o preço da pedra. No entanto, estas inclusões não a fazer perder o valor se são moderados, mas eles fazem das pedras, mais frágeis do que os outros para frisar. esmeraldas transparentes são, obviamente, muito popular mas uma esmeralda de um verde escuro, com poucas inclusões podem ser mais caras do que uma pedra transparente de um verde pálido.
Existem jazidas de esmeraldas na Colômbia, Brasil, Austrália, Índia, Zâmbia, Paquistão ...
A esmeralda tem sido uma pedra usada para jóias ornamentais desde a época do antigo Egito, ou seja, há 3.000 anos antes de nossa era. Havia muitas esmeraldas nos corredores e túmulos do Império egípcio.
A esmeralda era também uma pedra fetiches dos marajás; Por serem abundante na Índia. As esmeraldas eram também presentes nos principais reinos europeus. Um dos exemplares mais belos desta jóia, faz parte da coroa do Iran ». Napoleão ofereceu à Imperatriz Marie Louise, por ocasião do seu casamento, um conjunto de esmeraldas, incluindo uma tiara, um colar, um par de brincos e um pente. O vestido é agora propriedade do Louvre, em Paris.Não esquecendo o excelente exemplar à mostra no museu de Topkapi em stambul na Turquia.

EUA concedem primeira licença de exploração lunar privada

EUA concedem primeira licença de exploração lunar privada

A Agência Federal de Aviação (FAA) dos Estados Unidos autorizou uma empresa privada com sede na Flórida a realizar voos para a Lua com sondas robóticas, abrindo uma nova era de exploração do satélite terrestre. A companhia Moon Express, com base em Cabo Canaveral, recebeu a aprovação para enviar uma sonda com capacidade de alunissar e se reposicionar com pequenos “saltos”, informou nesta quarta-feira a organização.
“A FAA determinou que o lançamento da sonda não traz riscos para a saúde pública, para a segurança de pessoas e suas propriedades, para os interesses nacionais e de política externa, e para as obrigações internacionais”, disse a FAA em comunicado. A missão da Moon Express, batizada como MX-1E, tem a intenção de abrir um novo setor industrial, o de mineração lunar, com a extração de platina e hélio-3, o combustível para as usinas de fusão que ainda não existem e cuja viabilidade até agora só foi abordada pela ficção científica.
No entanto, com a autorização da FAA, a Moon Express se posiciona como favorita para ganhar o Google X Lunar Prize, o concurso no qual concorrem mais de uma dúzia de pequenas empresas com o objetivo de obter um prêmio de US$ 20 milhões. Este feito, mais administrativo do que tecnológico, representa a primeira vez que as autoridades americanas interpretam e aplicam o marco legal estipulado pelo Tratado do Espaço Exterior.
O acordo internacional determina que “as atividades de entidades não-governamentais no espaço exterior, incluída a Lua e outros corpos celestes, devem requerer autorização e contínua supervisão dos Estados-parte deste tratado”. A agência aeroespacial americana (Nasa), passou mais de quatro décadas, desde a missão Apolo 17, sem pôr os pés na Lua. A Nasa e o governo americano querem agora abrir a possibilidade para a participação da iniciativa privada na exploração espacial, como já ocorre com as missões de carga para a Estação Espacial Internacional.
Fonte: Exame

Anglo American anuncia nova mina de diamantes no Canadá

Anglo American anuncia nova mina de diamantes no Canadá

A Anglo American anunciou o comissionamento da mina de diamantes Gahcho Kué da De Beers nos territórios noroestes do Canadá. O ramp up da mina de Gahcho Kué é esperado para o primeiro trimestre de 2017. A expectativa é de uma produção média de 4,5 milhões de quilates anuais durante os 13 anos de vida útil da mina. Bruce Cleaver, CEO da De Beers disse que o ramp up da mina no prazo, orçamento e em um ambiente desafiador é um feito notável.
“A mina é um recurso excepcional em termos de volume de quilates e tem valor e potencial para criar oportunidades econômicas significativas para a comunidade envolvida”. A mina de Gahcho Kué é uma joint venture entre a De Beers (51%) e a Mountain Province Diamonds (49%).
Fonte: Brasil Mineral