Chapter 5: Minerals of Earths Crust By Julia Dovnarovich Period 4.
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Transcript of Chapter 5: Minerals of Earths Crust By Julia Dovnarovich Period 4.
Chapter 5: Minerals of Earth’s Crust
By Julia DovnarovichPeriod 4
What is a Mineral?
A mineral is a natural, usually inorganic solid that has a characteristic chemical composition, an orderly internal structure, and a characteristic set of physical properties.
Silicates• A silicate mineral is a mineral that contains a
combination of Silicon and Oxygen, and that may also contain one or more metals.
• 96% of Earth’s crust is made up of silicate minerals.
• Silicate minerals have 6 types of crystalline structures based on the arrangement of the Silicon-Oxygen tetrahedra.
Nonsilicates• A nonsilicate mineral is a mineral that does
not contain compounds of Silicon and Oxygen.
• Approximately 4% of Earth’s crust is made up of nonsilicate minerals.
• There are 6 major groups of nonsilicate minerals: Carbonates, Halides, Native Elements, Oxides, Sulfates and Sulfides.
Properties Used to Identify Minerals
1. Color2. Streak3. Luster4. Cleavage and Fracture5. Hardness6. Crystal Shape7. Density
Special Properties
• Fluorescence• Phosphorescence• Chatoyancy• Asterism• Double Refraction• Magnetism• Radioactivity