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A collection of identified rocks and minerals on display. The black stones on the left are obsidians; the lighter, hollow rocks are geodes.
A collection of identified rocks and minerals on display. The black stones on the left are obsidians; the lighter, hollow rocks are geodes.
A collection of smaller mineral samples stored and displayed in clear cases
A collection of smaller mineral samples stored and displayed in clear cases
Azurite specimen from the Morenci mine, Morenci, Arizona, USA. Morenci is the largest copper mine in North America, and Morenci copper mineral specime
Azurite specimen from the Morenci mine, Morenci, Arizona, USA. Morenci is the largest copper mine in North America, and Morenci copper mineral specimens are visually appealing, abundant, and relatively inexpensive.
Creedite specimen, 11 x 7 x 3 cm, from Santa Eulalia, Chihuahua, Mexico; formerly in the Perkins D. Sams collection
Creedite specimen, 11 x 7 x 3 cm, from Santa Eulalia, Chihuahua, Mexico; formerly in the Perkins D. Sams collection
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Page from Treatise on mineralogy by Friedrich Mohs (1825)
Page from Treatise on mineralogy by Friedrich Mohs (1825)
Calcite is a carbonate mineral (CaCO3) with a rhombohedral crystal structure.
Calcite is a carbonate mineral (CaCO3) with a rhombohedral crystal structure.
Aragonite is an orthorhombic polymorph of calcite.
Aragonite is an orthorhombic polymorph of calcite.
The perovskite crystal structure. The most abundant mineral in the Earth, bridgmanite, has this structure. Its chemical formula is (Mg,Fe)SiO3; the re
The perovskite crystal structure. The most abundant mineral in the Earth, bridgmanite, has this structure. Its chemical formula is (Mg,Fe)SiO3; the red spheres are oxygen, the blue spheres silicon and the green spheres magnesium or iron.