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Willemite

Willemite

A species of Phenakite Group, Also known as Villemite, Hebertine

Willemite is a stunning example of nature going over and above the call of beauty! It is one of the most well-known fluorescent minerals used in the production of some of the first versions of tubes for televisions. Without willemite, we may not be watching television today!

Hardness
Hardness:

5.5

Density
Density:

4.224 g/cm³

General Info About Willemite

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Physical Properties of Willemite

Luster
Vitreous, Resinous
Diaphaneity
Transparent to translucent
Colors
Colorless, white, pastel green, apple-green, light blue, azure-blue, yellow, burgundy-red, brown, mahogany-brown, gray, black, pink
Magnetism
Non-magnetic
Tenacity
Brittle
Cleavage
Good
Fracture
Uneven, Subconchoidal
Streak
White
Crystal System
Trigonal
Hardness
5.5 , Soft
Density
4.224 g/cm³, Obviously Heavy Weight
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Chemical Properties of Willemite

Chemical Classification
Silicates
Formula
Zn2SiO4
Elements listed
O, Si, Zn
Common Impurities
Al, Fe, Mn, Pb, Mg, Ca

Optical Properties of Willemite

Refractive Index
1.687-1.723
Birefringence
0.028-0.030
Pleochroism
None
Optical Character
Biaxial positive

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Rarity
Rare

Characteristics of Willemite

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Formation of Willemite

Willemite is usually formed as an alteration of previously existing sphalerite ore bodies, and is usually associated with limestone. It is also found in marble and may be the result of a metamorphism of earlier hemimorphite or smithsonite. Crystals have the form of hexagonal prisms terminated by rhombohedral planes: there are distinct cleavages parallel to the prism-faces and to the base. Granular and cleavage masses are of more common occurrence. It occurs in many places, but is best known from Arizona and the zinc, iron, manganese deposits at Franklin and Sterling Hill Mines in New Jersey. It often occurs with red zincite (zinc oxide) and franklinite (Fe,Mn,Zn)(Fe,Mn)2O4 (an iron rich zinc mineral occurring in sharp black isometric octahedral crystals and masses). Franklinite and zincite are not fluorescent.

Cultural Significance of Willemite

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Uses of Willemite

Willemite is an important ore of zinc, which is an essential metal used to produce batteries, paint, cosmetics, soaps, textiles, plastics, and much more. This mineral comes in many colors and has a wonderful fluorescence that makes it popular with collectors. However, willemite is too fragile for jewelry use.

Mineralogy and Petrology of Willemite

Willemite is usually formed as an alteration of previously existing sphalerite ore bodies, and is usually associated with limestone. It is also found in marble and may be the result of a metamorphism of earlier hemimorphite or smithsonite. Crystals have the form of hexagonal prisms terminated by rhombohedral planes: there are distinct cleavages parallel to the prism-faces and to the base. Granular and cleavage masses are of more common occurrence. It occurs in many places, but is best known from Arizona and the zinc, iron, manganese deposits at Franklin and Sterling Hill Mines in New Jersey. It often occurs with red zincite (zinc oxide) and franklinite (Fe,Mn,Zn)(Fe,Mn)2
O4
(an iron rich zinc mineral occurring in sharp black isometric octahedral crystals and masses). Franklinite and zincite are not fluorescent.

Etymology of Willemite

It was discovered in 1829 in the Belgian Vieille-Montagne mine. Armand Lévy was shown samples by a student at the university where he was teaching. Lévy named it after William I of the Netherlands (it is occasionally spelled villemite). The troostite variety is named after Dutch-American mineralogist Gerard Troost.

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