Scheelite is a mineral with a hardness of 5 out of 10 on the Mohs scale of mineral hardness [?]. These Tetragonally structured gems are made of calcium tungstate, their full chemical compound being CaWO4.

Scheelite is a mineral in the group of Sulfates, Chromates, Molybdates, Tungstates. It has the same crystal structure and outside appearance as powellite. But scheelite is a calcium-tungstate, while powellite is a calcium-molybdate.

In rocks, scheelite may appear as crystals like two pyramids connected at its bases, or pseudo-octahedral, or having table-like faces, with detectable parallel ridges on its surface. It is rare to find scheelite in granular masses, where it is white or yellowish (especially when molybdenum-bearing).


It is semi-hard, very heavy, fragile, with good cleavage that enables it to be split along even planes. It is translucent to transparent, with vitreous to adamantine luster. It is fluorescent in short wave ultraviolet light, giving off a pale blue light which turns yellow in the molybdenum-rich member of the scheelite group. It is soluble in acids and fuses with difficulty. Its double refraction makes scheelite easy to distinguish from other similar-looking stones.


It is yellow, green, or reddish-gray. The yellow color resembles the colored diamond. In unpolished form it looks like crystallized caramel.


Mineral and crystal growths occur in high-temperature pegmatitic and hydrothermal veins, in Alpine fissures and medium-grade metamorphic rocks, including some metamorphic rocks.


Side by side with scheelite in high temperature veins and pegmatites is the related mineral wolframite, a grey-black to brownish-black monoclinic mineral of high specific gravity, which itself is the principal ore of tungsten outside the USA.


Splendid crystals weighing half a kilogram are found in Brazil, but the most important economic masses occur in Bolivia, Burma, Malaysia, Japan, China, the USA, and Austria. Fine crystals up to 7.5 cm. (3 in.) are found at Traversella (Turin), in Val di Fiemme and Valsugana (Trento) in Italy, and in various localities in Sarrabus and Gerrei in Sardinia. Fine pseudomorphs of ferberite-heubnerite after scheelite have been found at Trumbull, Connecticut (USA).


Tungsten is an obsolete term for scheelite.


Scheelite can be confused with quartz, with which it is commonly associated, but is distinguished by the characteristic electric blue to yellow fluorescence under ultraviolet light.


It is sometimes used as a diamond substitute.


The specific gravity [?] for Scheelite is 6.1, it's refractive index [?] is 1.92-1.93, and it's double refraction [?] is 0.017.

History

Scheelite is named after Karl Wilhelm Scheele, the eighteenth century Swedish chemist who discovered 'tungsten,' which was the first name given to the stone by the Swedes. Scheelite was synthesized in the USA in 1963.

Industrial Usages

Scheelite is sometimes cut as very attractive faceted gems and prized by collectors. When dyed it can be confused with many gemstones. Cat's eye and four-rayed star scheelite are also known. It has also been manufactured synthetically.


Scheelite is an important ore of tungsten, especially in the USA. Tungsten is used to harden steels for use in high-speed tools and engine components, and to prepare tungsten carbides, abrasives which are second only to diamonds in hardness. Metallic tungsten has a high melting point - 3410°C (6170°F) - and is used in lamp filaments and spark plugs.

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Terms

Double Refraction or dr is the ability of a mineral to separate a refracted ray of light into 2 rays. If held over an image or text it will display the object 2x its original size.

Mohs Scale of Mineral Hardness is the standard used to categorize a mineral's ability to resist scratching. It gets its name from Friedrich Mohs, the German geologist who first created the scale.

RI or Refractive Index defines light's ability to move through the mineral or in a general sense, any material.

SG or Specific Gravity is the ratio of the weight of any substance to that of pure water at temperature of 3.98°C(39.2°F) and standard atmospheric pressure. This is important to note when actively seeking these minerals in the wild. Minerals with a higher SG will settle below material with a lower sg over time.