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By: Edward Liu
You have probably heard the word mineral before. Well,
     what are minerals? Some might say rocks, others might say
     gems, and both would be correct. Minerals are substances
     that:
1.   Has a crystalline structure
2.   Are naturally occurring
3.   Are nonliving
4.   Are solids
 There are two groups of minerals, the silicate and non-silicate.
 They are separated by their chemical composition.
 Silicates contain oxygen and silicon, the two most abundant
  elements in the Earth’s crust.
 About 90% of minerals are silicate.
 Most silicate minerals are a combination of an element mixed with
  silicon and oxygen.



                      +                    =
   Quartz – primary mineral that is in many rocks.


   Mica – minerals that separate into sheets.



 Feldspar – group of minerals that make up most of the Earth’s
crust.



   Olivine – common mineral in Earth’s subsurface.
   Non-silicate minerals are minerals that do not have a
    combination of oxygen and silicon in them.
   Non-silicate minerals include some elements.
   Non-silicate minerals are less common in the Earth’s crust
    than silicate minerals.




           X                                   X
   Native Elements: composed of one element. Copper, gold, silver, graphite,
    etc.


   Carbonates: contains combination of carbon and oxygen. Calcite, magnesite,
    etc.


   Halides: compounds formed when fluorine, chlorine, iodine, or bromine
    mixes with sodium, potassium, or calcium. Fluorite, halite, etc.


   Oxides: compounds formed when an element is chemically combined with
    oxygen. Ice, magnetite, corundum, etc.


    Note: Images are in the order in which they were listed in.
   Sulfates: minerals that have sulfur and oxygen in them. Gypsum, barite, etc.




   Sulfides: minerals that contain one or more elements. Galena, cobaltite, etc.
Minerals

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Minerals

  • 2. You have probably heard the word mineral before. Well, what are minerals? Some might say rocks, others might say gems, and both would be correct. Minerals are substances that: 1. Has a crystalline structure 2. Are naturally occurring 3. Are nonliving 4. Are solids
  • 3.  There are two groups of minerals, the silicate and non-silicate.  They are separated by their chemical composition.  Silicates contain oxygen and silicon, the two most abundant elements in the Earth’s crust.  About 90% of minerals are silicate.  Most silicate minerals are a combination of an element mixed with silicon and oxygen. + =
  • 4. Quartz – primary mineral that is in many rocks.  Mica – minerals that separate into sheets.  Feldspar – group of minerals that make up most of the Earth’s crust.  Olivine – common mineral in Earth’s subsurface.
  • 5. Non-silicate minerals are minerals that do not have a combination of oxygen and silicon in them.  Non-silicate minerals include some elements.  Non-silicate minerals are less common in the Earth’s crust than silicate minerals. X X
  • 6. Native Elements: composed of one element. Copper, gold, silver, graphite, etc.  Carbonates: contains combination of carbon and oxygen. Calcite, magnesite, etc.  Halides: compounds formed when fluorine, chlorine, iodine, or bromine mixes with sodium, potassium, or calcium. Fluorite, halite, etc.  Oxides: compounds formed when an element is chemically combined with oxygen. Ice, magnetite, corundum, etc. Note: Images are in the order in which they were listed in.
  • 7. Sulfates: minerals that have sulfur and oxygen in them. Gypsum, barite, etc.  Sulfides: minerals that contain one or more elements. Galena, cobaltite, etc.