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Published byBeverley Fox Modified over 8 years ago
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MINERALS
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Chemical composition of the Crust n Oxygen most abundant- 46.6% n Followed by silicon and aluminum n Iron, Calcium, Sodium, Potassium, Magnesium n The most common minerals will be composed mostly of these elements n Silica & silicates
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MINERAL vs. ROCK n ROCK u An aggregate of one or more MINERALS (usually- coal, organic) n MINERAL u Solid u Crystalline- orderly arrangement of atoms u Naturally occurring u Inorganic u Definite chemical composition F e.g. SiO 2 for quartz; KAlSi 3 O 8 for feldspar
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Atom & Elements n Atoms u Neutral u Nucleus F Proton, neutron u Electron n Ions u Electrical Charge n Molecule- e.g. water molecule
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Chemical activity n Stable atoms want u positive & negative charges balanced u electron shells full n Ions- positive (Cations) and negative (Anions) n Bonding u Ionic u Covalent u Metallic u Van der Waal’s
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Element n Atomic number u Number of PROTONS n Isotope u Differing number of NEUTRONS n Atomic weight u Mass of PROTONS and NEUTRONS
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Crystallinity n 3 dimensional orderliness of atoms n Silicon-oxygen tetrahedron n Silicate structures u Single- e.g. olivine u Chain F Single chain- pyroxene F Double chain- amphibole u Sheet- e.g. mica, clay u Framework- e.g. quartz, feldspar
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MINERALS n Crystalline solids n Natural and Inorganic Substances n Definite chemical composition u Can be written as a chemical formula u Solid solution (within a range)
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Important Minerals n Quartz (most abundant) n FELDSPAR Group u Potassium Feldspar - Orthoclase u Plagioclase Feldspar F Sodium (Na) Albite F Calcium (Ca) Anorthosite
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Important Minerals n PYROXENE Group- Augite most common n AMPHIBOLE Group- Hornblende most common n MICA Group- Si + O in sheets u Biotite u Muscovite n CALCITE- CaC O 3
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Properties of Minerals n Color u Not always reliable (Olivine, green; Flourite, yellow, purple, green…) u Ferromagnesian minerals green or black n Streak- powdered form n Luster- reflectance of light u Metallic u Nonmetallic F Vitreous or Glassy F Earthy
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Properties of Minerals n Hardness- resistance to scratching n Moh’s Hardness Scale u Fingernail = 2.5 u Penny = 3.5 u Knife/Glass = 5.5 u Streak Plate= 6.5 n Crystal Form u Law of Constancy of Interfacial Angles
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Properties of Minerals n Cleavage u Quality (poor, good, perfect) u Number of directions F One- e.g. Mica F Two at right angles- e.g. Feldspar, Pyroxene F Two not at right angles- e.g. Amphibole F Three at right angles (cubic)- e.g. Halite F Three not at right angles (rhombohedral)- e.g. calcite F Four (Flourite) or six (Sphalerite)- not common
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Properties of Minerals n Fracture u Absence of cleavage u Irregular fracture u Conchoidal fracture- Quartz n Density u Specific Gravity n Some unusual properties u Striations, Magnetism, Taste, Odor, Double refraction
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Chemical tests n Reaction with HCl u Calcite effervesces
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ROCK CYCLE n Equilibrium n Interrelationships between u igneous rocks u sediment u sedimentary rocks u metamorphic rocks u weathering and erosion n Plate Tectonic Example
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ROCK CYCLE n Equilibrium n Interrelationships between u igneous rocks u sediment u sedimentary rocks u metamorphic rocks u weathering and erosion n Plate Tectonic Example
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