Sphalerite Value, Price, and Jewelry Information
Sphalerite occurs in many colors, including green, yellow, orange, brown, and fiery red. With a dispersion over three times that of diamond and an adamantine luster, faceted specimens make beautiful additions to gem collections. However, they're too soft for most jewelry uses.
The International Gem Society (IGS) has a list of businesses offering gemstone appraisal services.
|Crystallography||Isometric. Crystals widespread, in various shapes; massive, cleavable, granular.|
|Colors||Colorless (very rarely); black (rich in Fe), brown, orange, yellow, green, orange-red, white-gray.|
|Luster||Resinous to adamantine.|
|Dispersion||0.156 (extremely high).|
|Luminescence||Bright orange-red to red in LW, SW, from many localities. Material from Otavi, Namibia is triboluminescent. (Produces light under friction).|
|Transparency||Transparent to opaque.|
|Absorption Spectrum||Sometimes 3 bands seen in the red at 6900, 6670, and 6510 due to cadmium.|
|Formula||ZnS + Fe|
|Optics||Isotropic; N = 2.37-2.50. (Spanish material 2.40).|
|Etymology||From the Greek sphaleros, meaning “treacherous,” because sphalerite often resembles galena (lead sulfide) but yields no lead.|
|Occurrence||Sphalerite is the chief ore of zinc, the most abundant zinc mineral, and is common in low-temperature ore deposits, especially in limestones; also in sedimentary rocks; hydrothermal ore veins.|
Iron-rich, opaque, black stones are known as marmatites, named after the locality, Marmato, Italy. In Europe, sphalerite is sometimes called blende, after the German word blenden, “to dazzle.” Though they have no connection to actual ruby gems, stones with red and orange shades are sometimes called “ruby blende.” Low-iron, pale and colorless sphalerites, known as cleiophanes, are extremely rare.
A number of trace elements may contribute to color in sphalerites. These include germanium, calcium, copper, mercury, and cerium (yellow); tin, silver, and molybdenum (reddish); and cobalt and iron (green).
Sphalerite and wurtzite are polymorphs. They share the same chemical formula (ZnS), but have different crystal habits. Sphalerite has an isometric crystal structure, while wurtzite has a hexagonal structure. These two minerals can coexist in alternating layers as schalenblende, a gem material used rarely for cabochons.
Sphalerites may have a streak color ranging from pale brown to yellow or white. Keep in mind that streak testing can destroy the test sample. Conduct this examination only as a last resort for gem identification on rough, never on a finished gem. This test will also release a sulfurous odor from the test sample.
Sphalerites are pyroelectric. When heated, these gems generate an electrical charge.
Since sphalerite ranks as the primary ore for zinc mining, scientists have synthesized this mineral for industrial research. In addition, facetable synthetic sphalerites in all their colors have appeared in jewelry and gem collections.
No known gemstone treatments.
Polishing scratches on the bottoms of sphalerite cabochons may cause apparent chatoyancy and asterism. (Although these scratches may occur accidentally, be aware that sphalerites don’t normally display these phenomenal effects).
Significant gem-quality sources include:
- Santander, Spain: major gem locality, large cleavages of red-orange color.
- Cananea, Sonora, Mexico: fine green transparent material, often pale colored and color zoned, sometimes yellow.
- Kipushi, Democratic Republic of the Congo: dark green material containing elevated amounts of cobalt and iron.
- United States: Franklin, New Jersey (almost colorless to pale green, transparent variety known as cleiophane); Kansas/Missouri/Oklahoma (so-called Tri-State Region, heavily mineralized by lead and zinc, with many localities and operating mines); Tiffin, Ohio (red color); Colorado/Utah (may be transparent); Arizona; Idaho; Montana; Wisconsin.
- Australia; Canada; China; Czech Republic; England; France; Germany; Tsumeb, Namibia; Romania; Scotland; Sweden
From the large, reddish material from Spain, faceters could easily cut gems of hundreds of carats, as well as cabochons. Green cleiophane material from New Jersey has yielded faceted gems as large as 15 carats. Mexican material could yield faceted gems to 50 carats.
- Smithsonian Institution (Washington, DC): 73.3, 68.9 (yellow-brown. Utah); 59.5 (yellow-green, New Jersey): 48 (yellow, Mexico); 61.9, 45.9 (yellow, Spain).
- California Academy of Sciences (San Francisco): 150.3 (dark red-brown oval, Spain).
- National Museums of Canada (Ottawa, Ontario): 100.1 (dark orange, round, Spain).
- Private Collection: 24.8 (gray-green, Mt. Ste. Hilaire, Quebec).
Clean sphalerites only with a soft brush, mild detergent, and warm water. See our Gemstone Jewelry Cleaning Guide for more recommendations.