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Minerals
                      • Natural
                      • Solid
                      • Inorganic
                      • Definite chemical
                        composition
                      • Crystal structure due
                        to internal
                        arrangement of atoms

http://www.minerals.net/gemstone/index.htm
General Facts about Minerals

• Between 2 - 3,000 have been identified
• A few are “native elements” -- made of
  only one element, such as sulfur, gold.
  copper, and graphite (carbon)
• Most are compounds, especially the
  silicate group (Si, O).
• Other important groups are oxides,
  carbonates, and sulfides.
Silica Tetrahedron
• Made up of one silicon atom (Si) and four
  oxygen atoms (O).
• Basis for most rocks on Earth.
Less than a dozen are common
         in most rocks
• Quartz                 • Olivine
• Feldspar (group)       • Amphibole (group)
• Muscovite (white       • Magnetite, limonite,
  mica)                    and other iron
• Biotite (black mica)     oxides
• Calcite                • Pyrite
• Pyroxene
Common uses include:
•   Aluminum--packaging, transport, building
•   Beryllium--gemstones, fluorescent lights
•   Copper--electric cables, wires, switches
•   Feldspar--glass and ceramics
•   Iron--buildings, automobiles, magnets
•   Calcite--toothpaste, construction
• http://www.mii.org/commonminerals.php
Minerals are identified by their
     key characteristics
    • Crystal Structure (form)
      • Cleavage vs fracture
      • Color – Least reliable
        • Streak – true color
            • Hardness
Moh’s Scale of Hardness

                    Finegernail – 2.5
                    Penny – 3.0


                    Glass – 5.0

                    Scratch Plate




           Diamond scratches everything!!
Mineral Identification (cont’d)
                 • luster
       • density (specific gravity)
          • special properties
                    --reaction to acid
  --fluorescence       --salty taste
               --magnetism
Crystal Structure (Form)
• External structure due to
  internal arrangement of
  the atoms
• Six basic groups of
  shapes, with about three
  dozen variations




  http://www.minerals.net/mineral/carbonat/aragonit/aragoni1.htm
Mineral cleavage/fracture

• Some minerals split along flat surfaces
  when struck hard--this is called mineral
  cleavage
• Other minerals break unevenly along rough
  or curved surfaces--this is called fracture
• A few minerals have both cleavage and
  fracture
Color                   • results from ability to
                                        absorb some
                                        wavelengths and
                                        reflect others
                                      • some minerals have
                                        characteristics
                                        colors
                                      • others vary due to
                                        chemical differences
                                        or impurities (atoms
                                        mixed inside the
                                        main elements)
http://www.minerals.net/mineral/carbonat/calcite/images/4assortd.htm
Streak
• Color of the powder
  when rubbed on a
  “streak plate”
  (unglazed porcelain)
• May be same as hand-
  specimen or different
• Some paint is based on
  powdered minerals
  (streaks).

http://www.minerals.net/mineral/oxides/hematite/hematit6.htm
Mineral Hardness
                                • Ability to scratch
                                  another mineral
                                • Mohs scale from 1
                                  (talc) to 10 (diamond)
                                • Quartz (most common
                                  mineral and most dust
                                  particles) is 7


http://mineral.galleries.com/minerals/elements/diamond/diamond.htm
• Describes how light
Luster                            reflects off the surface
                                • Main categories are
                                  “metallic” and “non-
                                  metallic”
                                • Non-metallic includes
                                  “dull,” glassy,”
                                  waxy,” “pearly,” and
                                  othershttp://www.min
                                  erals.net/mineral/sulfi
                                  des/pyrite/pyrite2.htm


http://www.minerals.net/mineral/sulfides/pyrite/pyrite2.htm
Density (Specific Gravity)
• All minerals have
  density (mass / volume),
  but some are very dense
• Examples include
  galena, magnetite, and
  gold
• Specific Gravity is the
  density of the mineral
  compared with density
  of water
   http://www.minerals.net/mineral/elements/gold/gold1.htm
Special Characteristics--
    the “Acid Test”
     Carbonates react
     with dilute HCl and
     other acids by
     fizzing or bubbling
     (releasing CO2 gas)
Special Characteristics--
          Fluorescence
                            • Some minerals will
                              glow when placed
                              under short-wave or
                              long-wave ultraviolet
                              rays
                            • Franklin and
                              Ogdensburg NJ are
                              famous for their
                              fluorescent minerals

http://www.sterlinghill.org/Tour%20information.htm
Special Characteristics--
                 Salty Taste
 • DO NOT TASTE
   MOST MINERALS!
 • Halite is the
   exception--it will
   taste salty




http://mineral.galleries.com/scripts/item.exe?LIST+Minerals+Halides+Halite
Special Characteristics--
              Magnetism
                               • Many iron minerals
                                 will produce an
                                 invisible magnetic
                                 force field
                               • “Lodestone” was
                                 used by Vikings
                                 more than 1,000
                                 years ago as
                                 compasses

http://www.minerals.net/mineral/oxides/magnetit/magneti4.htm
Useful Web Sites

•   www.mii.org
•   www.mineral.galleries.com/minerals
•   www.mineral.net
•   www.usgs.gov

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Minerals

  • 1. Minerals • Natural • Solid • Inorganic • Definite chemical composition • Crystal structure due to internal arrangement of atoms http://www.minerals.net/gemstone/index.htm
  • 2. General Facts about Minerals • Between 2 - 3,000 have been identified • A few are “native elements” -- made of only one element, such as sulfur, gold. copper, and graphite (carbon) • Most are compounds, especially the silicate group (Si, O). • Other important groups are oxides, carbonates, and sulfides.
  • 3. Silica Tetrahedron • Made up of one silicon atom (Si) and four oxygen atoms (O). • Basis for most rocks on Earth.
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  • 5. Less than a dozen are common in most rocks • Quartz • Olivine • Feldspar (group) • Amphibole (group) • Muscovite (white • Magnetite, limonite, mica) and other iron • Biotite (black mica) oxides • Calcite • Pyrite • Pyroxene
  • 6. Common uses include: • Aluminum--packaging, transport, building • Beryllium--gemstones, fluorescent lights • Copper--electric cables, wires, switches • Feldspar--glass and ceramics • Iron--buildings, automobiles, magnets • Calcite--toothpaste, construction • http://www.mii.org/commonminerals.php
  • 7. Minerals are identified by their key characteristics • Crystal Structure (form) • Cleavage vs fracture • Color – Least reliable • Streak – true color • Hardness
  • 8. Moh’s Scale of Hardness Finegernail – 2.5 Penny – 3.0 Glass – 5.0 Scratch Plate Diamond scratches everything!!
  • 9. Mineral Identification (cont’d) • luster • density (specific gravity) • special properties --reaction to acid --fluorescence --salty taste --magnetism
  • 10. Crystal Structure (Form) • External structure due to internal arrangement of the atoms • Six basic groups of shapes, with about three dozen variations http://www.minerals.net/mineral/carbonat/aragonit/aragoni1.htm
  • 11. Mineral cleavage/fracture • Some minerals split along flat surfaces when struck hard--this is called mineral cleavage • Other minerals break unevenly along rough or curved surfaces--this is called fracture • A few minerals have both cleavage and fracture
  • 12. Color • results from ability to absorb some wavelengths and reflect others • some minerals have characteristics colors • others vary due to chemical differences or impurities (atoms mixed inside the main elements) http://www.minerals.net/mineral/carbonat/calcite/images/4assortd.htm
  • 13. Streak • Color of the powder when rubbed on a “streak plate” (unglazed porcelain) • May be same as hand- specimen or different • Some paint is based on powdered minerals (streaks). http://www.minerals.net/mineral/oxides/hematite/hematit6.htm
  • 14. Mineral Hardness • Ability to scratch another mineral • Mohs scale from 1 (talc) to 10 (diamond) • Quartz (most common mineral and most dust particles) is 7 http://mineral.galleries.com/minerals/elements/diamond/diamond.htm
  • 15. • Describes how light Luster reflects off the surface • Main categories are “metallic” and “non- metallic” • Non-metallic includes “dull,” glassy,” waxy,” “pearly,” and othershttp://www.min erals.net/mineral/sulfi des/pyrite/pyrite2.htm http://www.minerals.net/mineral/sulfides/pyrite/pyrite2.htm
  • 16. Density (Specific Gravity) • All minerals have density (mass / volume), but some are very dense • Examples include galena, magnetite, and gold • Specific Gravity is the density of the mineral compared with density of water http://www.minerals.net/mineral/elements/gold/gold1.htm
  • 17. Special Characteristics-- the “Acid Test” Carbonates react with dilute HCl and other acids by fizzing or bubbling (releasing CO2 gas)
  • 18. Special Characteristics-- Fluorescence • Some minerals will glow when placed under short-wave or long-wave ultraviolet rays • Franklin and Ogdensburg NJ are famous for their fluorescent minerals http://www.sterlinghill.org/Tour%20information.htm
  • 19. Special Characteristics-- Salty Taste • DO NOT TASTE MOST MINERALS! • Halite is the exception--it will taste salty http://mineral.galleries.com/scripts/item.exe?LIST+Minerals+Halides+Halite
  • 20. Special Characteristics-- Magnetism • Many iron minerals will produce an invisible magnetic force field • “Lodestone” was used by Vikings more than 1,000 years ago as compasses http://www.minerals.net/mineral/oxides/magnetit/magneti4.htm
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  • 24. Useful Web Sites • www.mii.org • www.mineral.galleries.com/minerals • www.mineral.net • www.usgs.gov