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MINERALS
We are what we are!
Minerals
 Typical minerals
   Copper – Used in electrical wiring
   Gold – Used for jewelry
   Talc – Baby powder
   Quartz – The main ingredient in glass


 A rock can be defined as an aggregate of
 two or more minerals, but there are some
 exceptions.
Earth Mineral
 An earth mineral is…
   Naturally occurring
   Inorganic
   Solid
   Possesses an orderly internal structure




   Has a definite chemical composition
MINERAL GROUPS
RUBY, Garnet, Sapphire, etc.
Mineral Groups
 Silicates
   Silicone and Oxygen
 Non-silicates
   Carbonates
          Calcite & Dolomite

   Oxides
          Magnetite

   Sulfides
          Bornite

   Halides
          Fluoride

   Native Elements
          Diamond
Silicates

            Quartz               Oxygen




        Feldspar

                                Silicon

            Biotite   Silicon Tetrahedron

                      - The building block
                      of all Silicates.

       Hornblende
Silicate Subgroups
Ferromagnesian       Non-ferromagnesian
(dark)               (light)
Olivine              Light Mica
                     (Muscovite)
Pyroxene group       Orthoclase Feldspar
(Augite)
Amphibole group      Plagioclase Feldspar
(Hornblende)
Dark Mica            Quartz
(Biotite)
Non-silicates
 Carbonates
        Calcite & Dolomite
 Oxides
        Magnetite
 Sulfides
        Bornite
 Halides
        Fluoride
 Native Elements
        Diamond
PROPERTIES
Hardness, Cleavage, etc.
Crystal Form
 External expression of a mineral’s orderly
  internal arrangement of atoms.
 Examples
   Pyrite – Cubic




   Quartz – Hexagonal
Luster
 The quality of light reflected from the surface
  of a mineral.
 Examples
   Galena - Metallic




   Fluorite – Non-metallic
Types of Luster
 Metallic The mineral is opaque and reflects light
    as a metal would.
   Submetallic The mineral is opaque and dull. The
    mineral is dark
   Nonmetallic minerals are described using
    modifiers that refer to commonly known
    qualities.
   Waxy The mineral looks like paraffin or wax.
   Vitreous The mineral looks like broken glass.
   Resinous The mineral looks like hardened tree
    sap.
Color
 Unreliable
 Example
   Quartz
Streak
 Color of a mineral in its powdered form.
 Examples
   Mematite
     Oolitic
       Color - black
       Steak - black



     Sepoular
       Color - black
       Steak - black
Hardness
 The measure of the resistance of a mineral to
 scratching.

 Common testing materials
   Copper – 3.5
   Glass – 5.5
   Fingernail – 2.2
Hardness [Scale]
 Mineral               Moh’s Scale Rating
 Talc                  1
 Gypsum                2
 Calcite               3
 Fluorite              4
 Apatite               5
 Orthoclase Feldspar   6
 Quartz                7
 Topaz                 8
 Corundum              9
 Diamond               10
Cleavage
 Tendency of a mineral to break along planes
 of bonding

 Fracture describes the quality of the
 cleavage surface.
   fibrous ( dull, silky) fracture
   conchoidal (curved, shell-like lines) fracture
   irregular (rough, jagged) fracture
Cleavage Types
 Cubic Cleaves in three directions at 90° to
    one another
   Rhombohedral Cleaves in three directions
    but not at 90° to one another
   Octahedral Cleaves in four directions
   Dodecahedral Cleaves in six directions
   Basal Cleaves in one direction
   Prismatic Cleaves in two directions
Specific Gravity
 Specific Gravity of a mineral is a comparison
  or ratio of the weight of the mineral to the
  weight of an equal amount of water. The
  weight of the equal amount of water is
  found by finding the difference between the
  weight of the mineral in air and the weight of
  the mineral in water.
 The most common is 2.5 – 3
Others
 Taste
   Only soluble minerals have a taste, but it is very
   important that minerals not be placed in the
   mouth or on the tongue.
 Feel
 Magnetism
   Magnetism is the characteristic that allows a
   mineral to attract or repel other magnetic
   materials.
 Reaction to Acid

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Minerals ES

  • 2. Minerals  Typical minerals  Copper – Used in electrical wiring  Gold – Used for jewelry  Talc – Baby powder  Quartz – The main ingredient in glass  A rock can be defined as an aggregate of two or more minerals, but there are some exceptions.
  • 3. Earth Mineral  An earth mineral is…  Naturally occurring  Inorganic  Solid  Possesses an orderly internal structure  Has a definite chemical composition
  • 5. Mineral Groups  Silicates  Silicone and Oxygen  Non-silicates  Carbonates  Calcite & Dolomite  Oxides  Magnetite  Sulfides  Bornite  Halides  Fluoride  Native Elements  Diamond
  • 6. Silicates Quartz Oxygen Feldspar Silicon Biotite Silicon Tetrahedron - The building block of all Silicates. Hornblende
  • 7. Silicate Subgroups Ferromagnesian Non-ferromagnesian (dark) (light) Olivine Light Mica (Muscovite) Pyroxene group Orthoclase Feldspar (Augite) Amphibole group Plagioclase Feldspar (Hornblende) Dark Mica Quartz (Biotite)
  • 8. Non-silicates  Carbonates  Calcite & Dolomite  Oxides  Magnetite  Sulfides  Bornite  Halides  Fluoride  Native Elements  Diamond
  • 10. Crystal Form  External expression of a mineral’s orderly internal arrangement of atoms.  Examples  Pyrite – Cubic  Quartz – Hexagonal
  • 11. Luster  The quality of light reflected from the surface of a mineral.  Examples  Galena - Metallic  Fluorite – Non-metallic
  • 12. Types of Luster  Metallic The mineral is opaque and reflects light as a metal would.  Submetallic The mineral is opaque and dull. The mineral is dark  Nonmetallic minerals are described using modifiers that refer to commonly known qualities.  Waxy The mineral looks like paraffin or wax.  Vitreous The mineral looks like broken glass.  Resinous The mineral looks like hardened tree sap.
  • 14. Streak  Color of a mineral in its powdered form.  Examples  Mematite  Oolitic  Color - black  Steak - black  Sepoular  Color - black  Steak - black
  • 15. Hardness  The measure of the resistance of a mineral to scratching.  Common testing materials  Copper – 3.5  Glass – 5.5  Fingernail – 2.2
  • 16. Hardness [Scale] Mineral Moh’s Scale Rating Talc 1 Gypsum 2 Calcite 3 Fluorite 4 Apatite 5 Orthoclase Feldspar 6 Quartz 7 Topaz 8 Corundum 9 Diamond 10
  • 17. Cleavage  Tendency of a mineral to break along planes of bonding  Fracture describes the quality of the cleavage surface.  fibrous ( dull, silky) fracture  conchoidal (curved, shell-like lines) fracture  irregular (rough, jagged) fracture
  • 18. Cleavage Types  Cubic Cleaves in three directions at 90° to one another  Rhombohedral Cleaves in three directions but not at 90° to one another  Octahedral Cleaves in four directions  Dodecahedral Cleaves in six directions  Basal Cleaves in one direction  Prismatic Cleaves in two directions
  • 19. Specific Gravity  Specific Gravity of a mineral is a comparison or ratio of the weight of the mineral to the weight of an equal amount of water. The weight of the equal amount of water is found by finding the difference between the weight of the mineral in air and the weight of the mineral in water.  The most common is 2.5 – 3
  • 20. Others  Taste  Only soluble minerals have a taste, but it is very important that minerals not be placed in the mouth or on the tongue.  Feel  Magnetism  Magnetism is the characteristic that allows a mineral to attract or repel other magnetic materials.  Reaction to Acid