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Published byAmber Wilcox Modified over 9 years ago
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Ms Politano at Sterling Hill Mine
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Minerals Natural Solid Inorganic Definite chemical composition Crystal structure due to internal arrangement of atoms
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Minerals are identified by their key characteristics: Hardness crystal shape Luster Color Streak cleavage/fracture density (specific gravity) special properties
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Mineral Hardness Ability to scratch another mineral Mohs Scale of Hardness: Ranges from from 1 (talc) to 10 (diamond)
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Crystal Shape (Form) External structure due to internal arrangement of the atoms
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Luster Describes how light reflects off the surface Main categories are “metallic” and “non- metallic” Non-metallic includes “dull,” glassy,” waxy,” “pearly,” and other
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Color results from ability to absorb some wavelengths and reflect others some minerals have characteristics colors (Amethyst is often purple)
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Streak Color of the powder when rubbed on a “streak plate” (unglazed porcelain) May be same color as hand-specimen or different Some paint is based on powdered minerals (streaks).
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Mineral cleavage/fracture Some minerals split along flat surfaces when struck hard (looks like boxes or steps) this is called mineral cleavage Other minerals break unevenly along rough or curved surfaces--this is called fracture
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Cleavage
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Fracture
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Special Characteristics Acid Test Fluorescence Magnetism Smell and Taste (DON’T EVER TASTE A MINERAL UNLESS GIVEN SPECIFIC PERMISSION, YOU CAN GET VERY SICK)
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Fluorescence
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