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MINERALS Reese
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How do they form Minerals form when molten materials cools and hardens inside the Earth or on the surface. Sometimes minerals from when solutions with solutes evaporate.
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MINERALS Occur naturally and are inorganic solids (not alive).
Have crystalline structure.
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MINERALS Chemically minerals are elements or compounds.
Example: Gold is an element & a mineral. Example: NaCl is a compound & a mineral.
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MINERALS Rocks are made up of two or more minerals.
Example: Limestone is a rock made up minerals calcite & aragonite. Rocks can be minerals but not all minerals are rocks. Example: Cu is a mineral but is not a rock
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MINERALS There are about 3,000 minerals on Earth.
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BARITE
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CARBON
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QUARTZ
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GRAPHITE
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Copper
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FLUORITE
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MINERAL PROPERTIES
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LUSTER The way a mineral’s surface reflects light.
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LUSTER May vary from one sample to another sample of the same substance. Two major types of luster: Metallic Nonmetallic
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Metallic Luster
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Nonmetallic luster Earthy Luster Glassy
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Nonmetallic Pearly Luster
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COLOR Not very useful for identifying minerals whose color vary with the sample. Example: the colors of minerals quartz & fluorite vary with their samples. Quartz Fluorite
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COLOR Useful only for those minerals which always have the same color or very unique colors. Example: Malachite– green azurite----- blue
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SULFUR
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Malachite
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Azurite
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STREAK Color of a mineral in it powdered form.
Can be obtained by rubbing the mineral across a streak plate-- a piece of unglazed porcelain tile. Example: hematite always gives a reddish brown streak no matter what type of luster it displays.
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Streak Examples Hematite leaves a reddish brown streak.
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Streak Examples Pyrite leaves a greenish black streak.
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HARDNESS Ability of a mineral to resist scratching.
It is tested using the Mohs Hardness Scale.
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Mohs Hardness Scale Based on the fact that a harder mineral will scratch a softer one. Ten minerals are numbered from softest to hardest. Talc is the softest & has a value of 1. Diamond, the hardest of all minerals, has a value of 10.
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DENSITY Useful mineral identification property.
Used to determine the identity and purity of minerals. Pure mineral density is a constant value. Density = mass/volume. Example: gold and pyrite appear similar. Pyrite is often called “fool’s gold”. You can tell the two minerals apart by comparing their densities. Gold’s density: 19.3 g/cc Pyrite’s density: 5.01 g/cc
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