wulfenite
Wulfenite is a lead molybdate mineral with the chemical formula PbMoO4. It forms in the oxidized zones of lead-rich ore deposits, where it crystallizes from lead-bearing fluids as a secondary mineral. It is best known for its vivid orange, yellow, or red crystals, which are commonly tabular and can form thin plates or wedges. Wulfenite crystals are usually translucent to transparent with a vitreous luster and a Mohs hardness of about 3. Specific gravity is high, typically around 6.5 to 7.0, reflecting the lead content.
Wulfenite occurs worldwide in oxidized lead deposits. Notable sources include the Tsumeb deposit in Namibia and
Wulfenite was named after Franz Xaver von Wulfen, an 18th-century Austrian mineralogist. The mineral is primarily
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