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QUARTZ (SiO2) - Hardness=7 (harder than glass), no cleavage, density 2.7 g/cc, often translucent to transparent, but can occur in a variety of colors (pink=rose quartz, white=milky quartz, gray=smoky quartz, purple=amethyst), has a characteristic glassy luster; very resistant to weathering. Quartz is a silicate mineral. |
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FELDSPAR ((K,Na)AlSi3O8) and other compositions - Hardness=6 (harder than glass), two cleavage directions at approximately 90 degree angles, density 2.6-2.8 g/cc, wide variety of colors, but often white to fleshy pink; the most common mineral in igneous rocks. The feldspar minerals are in the silicate group. |
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CALCITE (CaCO3) - Hardness=3, three cleavage directions at approximately 75 degree angles, density 2.7 g/cc, commonly colorless to white or light yellow, reacts with dilute HCl; the mineral that most "sea shells" are made of and the primary constituent of the sedimentary rock limestone and the metamorphic rock marble. Calcite is a carbonate mineral. |
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HALITE (NaCl) - Hardness=2.5, three cleavage directions at 90 degree angles, density 2.1-2.6 g/cc, generally colorless to light yellow, brown, salty taste; a common evaporite mineral, ordinary table salt. Halite is a halide group mineral. |
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MUSCOVITE (KAl3Si3O10(OH)2) - Hardness=2-2.5, one perfect cleavage direction (peels off in thin sheets - one of the mica minerals), density 2.7-3.0 g/cc, colorless to light yellow or light brown; once used for windows. The micas are silicate minerals. |
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GYPSUM (CaSO4 . 2H2O) - Hardness=2 (softer than your fingernail), one good and two poor cleavage directions (often difficult to detect), density 2.3 g/cc, generally colorless to white; a common evaporite mineral and the primary component of "sheetrock". Gypsum is a sulfate mineral. |