- align=center bgcolor="#9966FF" | Uraninite | - align=center |
- align=center bgcolor="#9966FF" | General | - | Category | Mineral | - | Chemical formula | uranium oxide, UO2 | - align="center" bgcolor="#9966FF" | Identification | - | Colour | Black or brownish | - | Crystal habit | Massive, botryoidal, granular. Crystals uncommon. | - | Crystal system | Isometric | - | Cleavage | Indistinct | - | Fracture | Conchoidal to uneven | - | Mohs Scale hardness | 5 - 6 | - | Luster | Submetallic, greasy | - | Refractive index | Opaque | - | Pleochroism | None | - | Streak | Same as colour, black or brownish | - | Specific gravity | 7.5 - 10 | - | Fusibility | ? | - | Solubility | Soluble in sulfuric, nitric, and hydrofluoric acids. | - align="center" bgcolor="#9966FF" | Major varieties | - | Pitchblende | Massive | - |
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Uraninite is a major ore of uranium. An important occurrence of pitchblende is at Great Bear Lake in the Northwest Territories of Canada, where it is found in large quantities associated with silver. Some of the highest grade uranium occurrences in the world occur in the Athabasca Basin in northern Saskatchewan. It also occurs in Australia, Germany, England, and South Africa, and in New Hampshire, Connecticut, North Carolina, Wyoming, Colorado and New Mexico in the United States.
Uranium minerals | Oxide minerals
Pechblende | Pechblenda | Pechblende | Pitchblende | Uraninite | Uraninīts | Uraninitas | Uraniniet | bekblende | Blenda uranowa | Pechblenda | Настуран
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