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Chemical composition Zn2SiO4
Crystal system Trigonal
Habit prismatic; massive
Cleavage indistinct
Fracture Conchoidal to irregular
Hardness 5.5
Optic nature Uniaxial +
Refractive index 1.691 - 1.725
Birefringence 0.028
Dispersion n d
Specific gravity 3.89 - 4.19
Lustre Vitreous to resinous
Fluorescence green to yellow

Willemite was named after King Willem (William) the first (1772-1843) of The Netherlands, by the French mineralogist Armand Lévy whom discovered it in 1830 on former Dutch soil (present day Belgium).

Crystal Habit

crystals are long to short prismatic, to 10cm in length. Also fine to coarse granular massive.

Chemical Composition

Zinc silicate, Zn2Si04 . Minor to trace amounts of iron, aluminum, manganese, calcium and magnesium may be present.


Yellow to yellow-green shades of willemite can be confused with golden beryl (which possesses a lower refractive index at 1.570 - 1.575, is harder at 7.5 to 8, and has a lower specific gravity of 2.72), and chrysoberyl (which is harder at 8.5, has a higher specific gravity 3.73, and a higher refractive index at 1.746 – 1.755)


Transparent rough is colorless to golden yellow, pale blue-green. A canary-yellow variety of willemite from Tsumeb, Namibia has been documented, with the color attributed to cadmium (although whether the cadmium is present at a substitute for an essential component, or as finely divided greenockite – cadmium sulfide – is uncertain). Massive material cut en cabochon may be white, apple green, amethystine, yellow to golden brown, grayish, brown. An opaque flesh-red variety is called “troostite” which consists of exsolution laminae of willemite in tephroite, a manganese silicate.


may exhibit black inclusions of franklinite, an iron manganese zinc oxide.

Specific Gravity

3.89 – 4.19, sinks in all usual heavy liquids.

Refractive Index

nω = 1.691 – 1.694 , nε = 1.719 – 1.725


There are reports that some rough has been heat treated to convert it from colorless to blue.


The willemite from Franklin and Ogdensburg, Sussex County, New Jersey commonly fluoresces a brilliant green under Short Wave ultraviolet. It also commonly is phosphorescent, with some specimens continuing to luminesce for hours after excitation has terminated; triboluminscence (luminescence when the specimen is abraded or broken) has been observed. Willemite with a butter-yellow fluorescence has been observed but is uncommon at both Franklin and Ogdensburg. Fluorescent response in Namibian willemite appears to be more erratic in its presence or absence, and tends to be yellow under Short Wave ultraviolet radiation and yellow to orange under Long Wave. Fluorescence must not be considered diagnostic; non-fluorescent willemite has been observed. The “troostite” variety may appear as homogenous willemite in white light, but can exhibit thin lines or streaks of fluorescent green in a non-fluorescent groundmass.


None known


None known


Willemite occurs as a primary and secondary mineral in metamorphosed zinc ore deposits. It is uncommon, except at the zinc mines of Franklin and Ogdensburg in Sussex County, New Jersey, where it is one of the three primary ore minerals. Enormous tonnages were mined between circa 1830 and circa 1980. In the late 19th century, one crystal recovered yielded enough rough to cut several stones; the largest faceted stone was 8 carats and became part of the Frederick A. Canfield collection. Of willemite as a gemstone, Dunn (1995) writes: “Willemite has been cut as an uncommon, exotic gem. Fine-quality gemstones have been cut from orange-yellow willemite crystals: gems of 11.1 and 11.7 carats are in the Smithsonian Institution; one of 36.93 carats is in the Harvard Mineralogical Museum; and one of 6.28 carats is in the American Museum of Natural History in New York. Massive material may be quite clean internally and translucent and has provided some gemmy material for the cutting of cabochons.”Facet-grade willemite has also been recovered from the Tsumeb (Tsumcorp) Mine in Tsumeb, Namibia.

Care and Maintenance

Willemite can be decomposed by mineral acids into a colorless silica gel; care should be exercised in the use of chemical cleaning agents.


  • Anthony, John W., Bideaux, Richard A., Bladh, Kenneth W., and Nichols, Monte C. (1990): Handbook of Mineralogy: Mineral Data Publishing, Tucson, Arizona
  • Palache, C. (1935), Minerals of Franklin and Sterling Hill, New Jersey, USG Professional Paper 180
  • Palache, Charles, Harry Berman & Clifford Frondel (1944): The System of Mineralogy of James Dwight Dana and Edward Salisbury Dana Yale University 1837-1892, Seventh edition