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Lecture 3: Minerals Geol 101, J.S. Kite WVU, 2009 GEOL 102 Announcement: • Bring manual to lab EVERY week Mineral 7naturally occuring, solid inorganic element or compound of elements, ….. Spodumene Specimen from John Betts: www.johnbetts-fineminerals.com/index.htm Mineral 7naturally occuring, solid inorganic element or compound of elements, with a definite composition, or range of compositions, usually having regular internal crystalline structure. Watermelon Tourmaline has range in composition Objective for Today • Explain how chemistry works to form different mineral crystals with different properties. properties. • Example: carbon crystals – diamond vs. graphite Sources of Carbon Images Diamond by Joel Castellanos, ©1998 www.cs.unm.edu/~joel/CrystalLab/CrystalLab.html Graphite www.auburn.edu/~leeming/ graphite.jpg Physical Properties of Minerals • Chemical Composition • • • • • • • • Crystal Structure Cleavage Fracture Hardness Specific Gravity Color Streak Lustre Chemical Composition • Assume Some Chemistry Background, p. 32-38, Plummer & others, 2007, 11th ed. • Know Terms Like – Atomic Number – Atomic Weight ?H.S. Chemistry? • ~ atomic mass number – Electron, Proton, Neutron, Isotope, etc. • Symbols Textbook, Appendix C, p. A-7 Elements Building Blocks for Minerals, (Minerals Building Blocks for Rocks). Rocks). • 92 Natural Elements in the Universe (see Appendix D p. AA-8) • 99% of Universe is H, He Whole Earth Most Common Elements? • Fe (35% by weight or mass) • O (30%) • Si + Mg + Ni + 87 other elements = ~ 35 % Elements in Earth’s crust O = 47 % by wt.; 94 % by volume Si = 28 % by wt.; <1% by volume Al, Fe, Ca, Na, K, Mg: 2-8% each) Rest ~ 1.5% total (See p. 38 in Plummer & others, 2007) 2 Models of the Atom Most elements occur as ions. • Ions: Ions: Atoms with Unbalanced Number of Protons (+) & Electrons ((-) • Valence: Valence: Combining Capacity e.g. H2O H+ & H+ & O-2 • Cation (+ charged ion) • Anion ((- charged ion) Atoms of Two “Inert” Elements Electron # = Proton # Valence: Valence: Combining Capacity H2 O Molecule Chemical Composition • Most Properties are Determined by Chemistry • Minerals Classified by Chemistry • Read Textbook: Textbook: p. 3333-43 in Plummer & others, 2007) Mineral Classes • Silicates (SiO4)-4 Quartz (SiO2), Garnets, Micas, Feldspars • Other Mineral Groups Quartz Garnet – Oxides O-2 – Sulfides S-4 – Carbonates (CO3)-2 – Halides Cl- • Mineraloids – Lack “xl” structure Images from John Betts: www.johnbetts-fineminerals.com/index.htm K-Feldspar & Quartz Mineral Classes • Silicates (SiO4)-4 • Oxides O-2 –Hematite (Fe2O3) & Limonite: Iron Oxide (Rust) • • • • • Sulfides S-4 Carbonates (CO3)-2 Halides ClOther Mineral Groups Mineraloids Matt Goff’s Toyota Pickup www.nawwal.org/~mrgoff/pictures/ misc/pickup2.jpg Mineral Classes • Silicates (SiO4)-4 • Oxides O-2 • Sulfides S-4 –Pyrite (FeS2): =Fool’s Gold • • • • Carbonates (CO3)-2 Halides ClOther Mineral Groups Mineraloids Mineral Classes • Silicates (SiO4)-4 • Oxides O-2 • Sulfides S-4 • Carbonates (CO3)-2 –Calcite (CaCO3) Calcite Image from John Betts: www.johnbetts-fineminerals.com/index.htm Mineral Classes • • • • Silicates (SiO4)-4 Oxides O-2 Sulfides S-4 Carbonates (CO3)-2 • Halides Cl- Br- Fl- etc. –Halite (NaCl): Rock Salt • Other Mineral Groups • Mineraloids Mineral Classes • • • • • Silicates (SiO4)-4 Oxides O-2 Sulfides S-4 Carbonates (CO3)-2 Halides Cl- • Other Mineral Groups – Weird Stuff Image from John Betts: • Mineraloids www.johnbettsfineminerals.com/index.htm Mineral Classes • • • • • • Silicates (SiO4)-4 Oxides O-2 Sulfides S-4 Carbonates (CO3)-2 Halides ClOther Mineral Groups • Mineraloids –No Xline Structure –e.g. Opal, Agate Agate Physical Properties of Minerals • Chemical Composition • Crystal Structure • • • • • • • Cleavage Fracture Hardness Specific Gravity Color Streak Lustre Valence & Size of Combining Atoms Determine a Mineral’s Crystal Structure Crystal (xl) • Solid with an Orderly Atomic Arrangement, • Which May Develop External Faces that Give the Crystal Form Halite (NaCl) Crystal Lattice • 3D Arrangement of Atoms within a Mineral Galena Crystal Lattice Unit Cell • Smallest Unit of 3D Arrangement for a Mineral Types of Bonds, p. 36 in Plummer et al. 2007 Textbook Ionic + or - Valence Attraction Carbon in 2 forms: diamond w/ covalent bonds, graphite w/ van der Walls bonds Types of Bonds, p. 36 in Plummer et al. 2007 Textbook Ionic + or - Valence Attraction Covalent Shared Electrons Metallic Free Electrons Carbon in 2 forms: diamond w/ covalent bonds, graphite w/ van der Walls bonds Van Der Waals (not in book): book): Weak Electrostatic Attraction Quartz Amethyst Cut Amethyst (Quartz) Maine Geological Survey Amethyst Images Source: Maine Geological Survey Si Tetrahedral Layers (SiO2) Triangular Pyramid Si4+ in Center O2- at Nodes # Slides Marked with # Were Taken In Part From This Web Site: An Insiders Look at the Silicates Natural History Museum of Los Angeles County http://www.nhm.org/lacmnh/departments/ research/mineralogy/silicates/index.htm Si Tetrahedral Layers (SiO2) # Minerals Olivine, Garnets Silicate Groups See Textbook p. 38-39 Pyroxenes Amphiboles Micas, Clays Quartz, Feldspars Structure Al(OH)3 or Al Octahedron Al OH- # Van Der Waals Bonds on Sheet Sillicate Physical Properties of Minerals • Chemical Composition • Crystal Structure • Cleavage • • • • • • Fracture Hardness Specific Gravity Color Streak Lustre Cleavage • Tendency for a Mineral to Break Along a Plane of Weakness Van Der Waals Bonds in Mica Cleavage: Flourite & Feldspar Physical Properties of Minerals • Chemical Composition • Crystal Structure • Cleavage • Fracture • • • • • Hardness Specific Gravity Color Streak Lustre Fracture Any Breaking Not Along a Plane of Weakness Conchoidal Fracture in Malachite Physical Properties of Minerals • • • • Chemical Composition Crystal Structure Cleavage Fracture • Hardness = Scratchability • • • • Specific Gravity Color Streak Lustre Mohs (1822) Hardness Scale 1. 2. 3. 4. 5. 6. 7. 8. 9. 10. Talc Gypsum Calcite Fluorite Apatite Orthoclase Quartz Topaz Corundum Diamond Hardness Scale • • • • • fingernail = 2.5 copper penny = 3.5 pocket knife = 5.5 glass = 5.5 steel file = 6.5 Physical Properties of Minerals • • • • • Chemical Composition Crystal Structure Cleavage Fracture Hardness • Specific Gravity • Color • Streak • Lustre Specific Gravity Mineral Mass/Volume g/cm3 water 1.000 ice 0.917 most minerals 2.0 to 4.0 galena 7.5 gold 19.3 Physical Properties of Minerals • • • • • • Chemical Composition Crystal Structure Cleavage Fracture Hardness Specific Gravity • Color • Streak • Lustre Color • Obvious for Few Minerals • Inconsistent • Minor Atomic Substitutions Give Great Variety of Color to One Mineral Quartz = Amethest Corundum = Ruby Physical Properties of Minerals • • • • • • • Chemical Composition Crystal Structure Cleavage Fracture Hardness Specific Gravity Color • Streak • Lustre STREAK COLOR OF POWDER MORE CONSISTENT THAN CRYSTAL COLOR Hematite: Reddish Brown Streak Physical Properties of Minerals • • • • • • • • Chemical Composition Crystal Structure Cleavage Fracture Hardness Specific Gravity Color Streak • Lustre Lustre • Metallic • Nonmetallic – Dull – Glassy – Pearly – Adamantine Other Physical Properties Specific to Few Minerals, may be Diagnostic Calcite: - ExamplesNormal Light ¾Magnetism ¾Reaction to HCl ¾Fluorescence (UV Light) Calcite: UV Light Rock solid cohesive aggregate of grains of one or more minerals.