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Structure and Formation of Minerals
4.2 Mineral Formation Structure and Formation of Minerals
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Learning Targets: Describe how melted rock produces minerals
Describe how hot rock produces different minerals Explain how minerals form from solutions
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Mineral Formation Minerals form by: Formation from Hot Material
Formation from Solutions Formation from Hot Underground Water
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Formation from Hot Material
Magma is molten rock Molten = melted Underground Magma Above ground Lava Most magma never becomes lava, it cools underground
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Magma cooling underground
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Cooling of Magma When magma cools, it solidifies
Cool Solidify Crystallize Rocks: mixture of minerals Magma can solidify in seconds or over millions of years Crystal is a pure mineral
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Cooling of Magma Quick cooling = small crystals
Atoms do not have time to arrange themselves Slow cooling = large crystals Atoms arrange and rearrange themselves until they are in the most stable positions
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Small minerals Feldspar in the cracks
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Large minerals Large feldspar
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Very large minerals
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Cooling of Magma Magma cools slowly; lava cools quickly
Lava traps more gas as it cools Sometimes lava cools so quickly no crystalline structure can develop
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Formations from Solutions
Water in nature always contains some amount of minerals it is a solution Hot water holds more minerals Minerals can precipitate out of solution Precipitate: water evaporates but minerals are left behind Salts are most common
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Halite: Rock Salt
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Minerals from Hot Underground Water
Water deep below the surface can be very hot Hot water = more minerals As water moves up through cracks in rocks Water cools minerals are deposited Hot water = minerals dissolve Cold water = minerals precipitate
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Mineral Rich Water When water deposits minerals into cracks in existing rock, veins are formed
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Quartz Vein
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Gold bearing vein in brown
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Vein with a fault
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