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Earth

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There are approximately 4000 known minerals (some common, some rare) ... The streak is the color of freshly crushed mineral powder and is usually constant. ... – PowerPoint PPT presentation

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Title: Earth


1
Earths Materials
  • Minerals The building blocks of the Earth

2
Minerals
  • Minerals are substances which are
  • Naturally occurring
  • Solid
  • Inorganic
  • Definite composition
  • Definite atomic arrangement

3
Minerals
  • There are approximately 4000 known minerals (some
    common, some rare)
  • All are compounds of elements.
  • Most minerals are composed of 8 elements

4
Common Elements of Earths Crust
Name Element Symbol Percent by mass (crust)
Oxygen O 46.6
Silicon Si 27.7
Aluminum Al 8.1
Iron Fe 5.0
Calcium Ca 3.6
Sodium Na 2.8
Potassium K 2.6
Magnesium Mg 2.1
Other 1.5
5
Mineral Properties and Identification
(Reference Tables)
  • Luster Metallic or non-metallic
  • The way light shines off a fresh surface of the
    mineral
  • Most minerals are non-metallic

6
Mineral Properties/ID
  • Hardness
  • The resistance a mineral has to being scratched

7
Mohs Hardness Scale
8
Mineral Properties/ID
  • Cleavage/Fracture
  • Cleavage is the tendency of a mineral to break
    along zones of weakness and form smooth, parallel
    sides.
  • Fracture is the tendency of a mineral to break in
    random directions

9
Mineral Properties/ID
  • Color and Streak
  • The color of a mineral can be useful, HOWEVER, it
    can vary due to slight chemical differences
  • The streak is the color of freshly crushed
    mineral powder and is usually constant.

10
Mineral Properties/ID
  • Using the Reference Tables

11
Mineral Formation 1
  • From Magma (molten rock)
  • Magma (very hot) begins to cool
  • As the magma cools, atoms and molecules begin for
    form compounds
  • Compounds merge together to form mineral grains
  • Many different minerals can form out of one
    batch of magma

12
Mineral Formation 2
  • Recrystalization
  • A rock is subjected to high temperature and
    pressure
  • Some minerals begin to chemically change without
    melting
  • Atoms and molecules recombine in a new way and
    minerals begin to grow
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