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CategoryMolybdate minerals
(repeating unit)
Strunz classification7.GA.05
Crystal systemTetragonal
Crystal classDipyramidal (4/m)
(same H-M symbol)
Space groupI41/a
Unit cella = 5.222 Å,
c = 11.425 Å; Z = 4
Formula mass200.02 g/mol
ColorStraw-yellow, greenish yellow, yellow-brown, brown, colorless, may show blue to black zones
Crystal habitFlat tabular crystals often paper-thin on {001}, may be crusty to pulverulent or massive
CleavageIndistinct on {011}, {112} and {001}
Mohs scale hardness3.5-4
Streaklight yellow
Specific gravity4.25
Optical propertiesUniaxial (+)
Refractive indexn? = 1.974 n? = 1.984
Birefringence? = 0.010
PleochroismO = blue; E = green
Ultraviolet fluorescenceFluoresces bright yellow under shortwave ultraviolet light, dimmer under longwave

Powellite is a calcium molybdate mineral with formula CaMoO4. Powellite crystallizes with tetragonal - dipyramidal crystal structure as transparent adamantine blue, greenish brown, yellow to grey typically anhedral forms. It exhibits distinct cleavage and has a brittle to conchoidal fracture. It has a Mohs hardness of 3.5 to 4 and a specific gravity of 4.25. It forms a solid solution series with scheelite (calcium tungstate, CaWO4). It has refractive index values of n?=1.974 and n?=1.984.[2]

Powellite was first described by William Harlow Melville in 1891 for an occurrence in the Peacock Mine, Adams County, Idaho and named for American explorer and geologist, John Wesley Powell (1834-1902).[2]

It occurs in hydrothermal ore deposits of molybdenum within the near surface oxidized zones. It also appears as a rare mineral phase in pegmatite, tactite and basalt. Minerals found in association with powellite include molybdenite, ferrimolybdite, stilbite, laumontite and apophyllite.[4]


  • Palache, C., H. Berman, and C. Frondel (1951) Dana's System of Mineralogy, (7th edition), v. II, pp. 1079-1081.

External links

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