Red Cloud (closed) historical premium. Mexican orange tablets mid.
Approximate retail prices. Wholesale + private sale typically 40-60% of retail. Auction premium 10-25%. For investment-grade purchase steps, see the investment checklist.
Elemental Composition (by mass)
Element
Mass %
Visual
PbLead
56.44%
MoMolybdenum
26.13%
OOxygen
17.43%
Computed from simplified end-member formula. Solid-solution series, water content, and trace substitutions cause real-world variation.
IMA Abbreviation (Whitney-Evans 2010)
Wul
→ Wulfenite
Pb molybdate
Standard symbol from American Mineralogist (Whitney & Evans, 2010). Used in thin-section labeling, phase diagrams, and IMA-style species records.
Pronunciation
/ˈwʊlfənaɪt/
↔ WOOLF-uh-nite
for F.X. von Wulfen
⚠ Safety & Handling
☠toxicmoderate
Lead molybdate.
Handling: Wash hands.
Information provided in good faith. Consult local hazmat regulations for transport and disposal. Severely hazardous specimens may require special storage cabinets.
Tenacity
Behavior:
brittle (fragile)
Under stress:
Thin plates chip easily
Tabular crystals very thin; chip on edges.
Luster
adamantine→resinous
Bright orange-yellow with characteristic adamantine sparkle.
Wulfenite (PbMoO₄) is a lead-molybdate mineral famous for its bright orange, yellow, and red square tabular crystals. The most prized Wulfenite specimens — saturated honey-orange paper-thin tablets from Red Cloud Mine (Arizona) and Mibladen (Morocco) — are among the most photographed minerals in collector literature.
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Wulfenite (PbMoO₄) is a lead-molybdate mineral famous for its bright orange, yellow, and red square tabular crystals. The most prized Wulfenite specimens — saturated honey-orange paper-thin tablets from Red Cloud Mine (Arizona) and Mibladen (Morocco) — are among the most photographed minerals in collector literature. China hosts modest Wulfenite occurrences at Yongping (Jiangxi).
Wulfenite typically forms tabular square platelets (often paper-thin); pyramidal; massive. Its color range is broad, including orange, orange-red, yellow, honey-yellow, gray, brown, white, and olive-green. The luster is adamantine, resinous, sub-adamantine, the streak is white, and specimens range from transparent to translucent. The cleavage is distinct on {001}. The fracture is uneven to conchoidal, which aids identification.
Collector context
How it forms
The geological setting for Wulfenite is typically secondary mineral in oxidized zones of lead ore deposits. It is commonly found in association with mimetite, cerussite, vanadinite, dioptase, fluorite, calcite.
Classic Chinese localities
**Dexing Cu-Mo-Au ore field** is an important Chinese source for the species.
Why collectors care
Wulfenite is a frequently-sought species in serious collections because its habit is recognizable, its color often strong, and its best examples unmistakable even at a distance. Chinese material has driven much of the recent visual shift in the species — sharper crystals, deeper colors, cleaner matrix.
What affects value
Value in Wulfenite is assessed, in typical order of weight, against: (1) locality provenance; (2) size relative to the species norm; (3) crystal form and termination sharpness; (4) color saturation and zoning; (5) transparency and internal clarity; (6) matrix quality and aesthetic balance; (7) condition (absence of damage, chips, or repair). Cleaning quality and verified locality documentation act as multipliers across the above.
Naming history
The name Wulfenite has a specific etymological and historical context — see Mindat's reference entry for provenance details. We have retained naming data at the record level; published prose is paraphrased from factual fields rather than copied from source.
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