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GSCI 340 - Environmental Geology
Fort Hays State University
Spring 2011

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Lecture #5

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Clerical:

  • Quizzes 1-4 are posted.
  • The Exam #1 Study Guide is posted.

    Themes of the Day:

    • Minerals Defined
    • Basic Chemistry Review
    • Chemical Bonding and Crystalline Structures
    • Physical Properties
    • Important Minerals

    Minerals Defined

    • Definition
      • Occurs Naturally
      • Inorganic
      • Solid
      • Characteristic Chemical Formula
      • Crystalline Structure
    • Mineral - Yes or No? Examples: coal (Kentucky's state "mineral"), cubic zirconia, pearl, mercury, glacier ice, volcanic glass, etc.

    Musical Interlude: The Elements by Tom Lehrer (music by Sir Arthur Sullivan). Sing along!
    Now also available in a Flash animation!!!

    Basic Chemistry Review

    • Minerals are built from atoms that are chemically bonded together in crystalline lattices.
    • The Atom: Nucleus (Protons, Neutrons), Electrons
    • Isotopes (variable numbers of neutrons) used for isotopic age dating
    • Ions - charged atoms with # of electrons not equal to # of protons - important for bonding
      • Anions - negative charge - # of Electrons > # of Protons - ex. Chlorine (Cl-), Oxygen (O2-)
      • Cations - positive charge - # of Electrons < # of Protons - ex. Sodium (Na+), Magnesium (Mg2+)
    • Periodic Table - helps predict ionic charges
    • Ions with similar charges and sizes may substitute for each other in some minerals
    • Abundance of elements in the Earth's crust:
      Element Chemical Symbol and
      Common Ion(s)
      Percent
      (by weight)
      Oxygen O2- 46
      Silicon Si4+ 28
      Aluminum Al3+ 8
      Iron Fe2+ or Fe3+ 6
      Magnesium Mg2+ 4
      Calcium Ca2+ 2.4
      Potassium K1+ 2.3
      Sodium Na1+ 2.1
      All others
      <1

    Chemical Bonding and Crystalline Structures

    • Bonding is what happens when ions share electrons.
    • Four basic types
      • Ionic bonds - electron(s) completely transferred - e.g., Halite (NaCl) - tend to be brittle bonds
      • Covalent bonds - electron(s) more evenly shared - e.g., Diamond (C) - strong bonds (diamond is strongest)
      • Metallic bonds - transition metal nuclei swimming in a sea of shared electrons - e.g., Gold (Au) - malleable
      • Intramolecular bonds - including hydrogen bonds and Van der Waals bonds - generally weak (often feels greasy) - e.g., graphite (C) or talc (Mg3AlSi3O10(OH)2)
    • Silicate minerals, containing covalently bonded SiO4 tetrahedra are most common in Earth's crust and mantle - subclassification system for silicates based on linkages of the SiO4 tetrahedra
    • Unit Cell - smallest building block that has all of a mineral's structural and chemical characteristics
    • Crystal Systems - mineral groupings based on internal symmetry - sometimes reflected in ideal crystal shapes - e.g. quartz and ice belong to the Hexagonal crystal system, halite is cubic
    • Bond types and crystaline structure are directly related to physical properties (see below) - e.g. Diamond & Graphite

    Physical Properties

    • Habit - naturally occuring shape of crystals
    • Cleavage - planar surfaces along which a mineral tends to break preferentially (related to weak bonding planes within a mineral's crystal structure - e.g., micas, halite, pyroxenes &amphiboles
    • Fracture - non-planar breakage behavior of a mineral - e.g., choncoidal fracture in glass or quartz
    • Hardness - resistance to scratching (also reflects bond strength) - Mohs' Hardenss scale
    • Specific Gravity - very similar to density
    • Color - often distinctive, sometimes variable or unreliable
    • Streak - color of powdered mineral - not always the same as color of unpowdered mineral
    • Luster - degree of reflectivity - e.g., galena - metallic, quartz - glassy, chalk - dull or earthy
    • Special Properties:
      • Magnetism - a magnet is attracted to the mineral magnetite (Fe3O4)
      • Aroma (odor) - some sulfur-bearing minerals stink like rotten eggs when scratched
      • Taste - halite (NaCl - rock salt) tastes salty (duh!)
      • Acid Reaction - calcite (CaCO3 - the mineral that makes up limestone) effervesces when you drop acid on it

    Important Minerals

    • Common Rock-Forming Minerals - mostly silicates
        Igneous Rocks
      • Ferromagnesian Minerals - Olivine, Pyroxene, Amphibole, Biotite - Dark in color, common in mafic rocks
      • Feldspars - Plagioclase, Orthoclase (K-feldspar)
      • Quartz
        Sedimentary Rocks
      • Quartz & Feldspar
      • Clay Minerals
      • Carbonate Minerals - Calcite & Dolomite
      • Evaporite Minerals - Halite, Gypsum
        Metamorphic Rocks
      • Most of the above, plus:
      • Micas, Garnet, Aluminosilicate Polymorphs (Andalusite, Kyanite, Sillimanite), and many more...
    • Ore and Industrial Minerals
      • Native Elements - Gold, Silver, Copper, Sulfur, Graphite, Diamond
      • Oxides - Iron Oxides (Hematite, Magnetite, Limonite), Chromite, others
      • Hydroxides - Bauxite (aluminum ore)
      • Sulfides - many metal ores (Cu, Pb, Zn, Mo, Hg, Ni, etc.) - potential environmental hazards in mining and refining
      • Sulfates - Gypsum (main constituent of Sheetrock), Barite (drilling muds)
      • Halides - Halite (rock salt - many uses), Sylvite (K for fertilizer), Fluorite (Fluorine)
      • Carbonates - Calcite (many uses)
      • Phosphates - Apatite (P for fertilizer)
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    GSCI 340 - Environmental Geology
    Dr. Ron Schott, Assistant Professor of Geology
    Fort Hays State University - Geosciences Dept.
    600 Park Street, Hays, KS  67601-4099
    Phone: (785)628-5348  Fax: (785)628-4096
    E-mail: rschott@fhsu.edu
    Web: http://hays.outcrop.org/schott/
    Page content last revised on: 27 January 2011