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:
5.5
Density:
4.224 g/cm³
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Properties
Values
Characteristics
Cultural
Common Questions
General Info About Willemite
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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.
Common Questions People Also Ask
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