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Minerals and Rocks An introduction to Geology: Mineralogy and Petrology
Minerals A mineral is a naturally occurring solid with a specific chemical composition and atomic arrangement (crystalline structure).* Quartz = Silica + Oxygen or SiO2 * Some references also add “inorganic” to the definition, but there are some rare organic minerals too (i.e., whewillite).
Methods to Identify Minerals Color Streak Luster Fluorescence Chemical Composition Hardness Talc Gypsum Calcite Fluorite Apatite Orthoclase Quartz Topaz Corundum Diamond ( Mnemonic Devise - The Geologist Can Find An Ordinary Quartz Tourists Call Diamond) Specific Gravity Crystal Form Optical Properties Cleavage Fracture Magnetism Electrical Properties Melting Point Geologic Setting
        Copper
Gold
Pyrite  (Fool’s Gold)
             Arsenic
       Bauxite (aluminum ore)
          Kaolin Mine Near Thomson, Georgia
Barite (rose morphology)
         Quartz
        ROCKS ,[object Object]
There are three primary types of rocks:Sedimentary Igneous Metamorphic
SEDIMENTARY ROCKS Rocks formed from accumulation and hardening of water or airborne sediment, plant or animal remains, chemical action, or evaporation. Some of the most common sedimentary rocks are: ,[object Object]
 Shale
 Sandstone,[object Object]
Limestone with fossils
          Shale
   Sandstone
       Peat Coal
                   Igneous Rocks ,[object Object]
  There are two main categories of igneous 	rocks:Intrusive – formed underground Extrusive – formed above ground
The most common intrusive igneous rock is granite. Some common extrusive igneous rocks include: ,[object Object]
  Obsidian
 Pumice,[object Object]
    ←  Obsidian              Pumice  ->
Basalt – vesicular (with holes), dense, and thin-section
Metamorphic Rocks These rocks are formed by other rocks being buried deep within the earth and subjected to very high temperature and pressure. Common metamorphic rocks include: ,[object Object]
  Greenstone

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Min Pet Presentation

  • 1. Minerals and Rocks An introduction to Geology: Mineralogy and Petrology
  • 2. Minerals A mineral is a naturally occurring solid with a specific chemical composition and atomic arrangement (crystalline structure).* Quartz = Silica + Oxygen or SiO2 * Some references also add “inorganic” to the definition, but there are some rare organic minerals too (i.e., whewillite).
  • 3. Methods to Identify Minerals Color Streak Luster Fluorescence Chemical Composition Hardness Talc Gypsum Calcite Fluorite Apatite Orthoclase Quartz Topaz Corundum Diamond ( Mnemonic Devise - The Geologist Can Find An Ordinary Quartz Tourists Call Diamond) Specific Gravity Crystal Form Optical Properties Cleavage Fracture Magnetism Electrical Properties Melting Point Geologic Setting
  • 4. Copper
  • 7. Arsenic
  • 8. Bauxite (aluminum ore)
  • 9. Kaolin Mine Near Thomson, Georgia
  • 11. Quartz
  • 12.
  • 13. There are three primary types of rocks:Sedimentary Igneous Metamorphic
  • 14.
  • 16.
  • 18. Shale
  • 19. Sandstone
  • 20. Peat Coal
  • 21.
  • 22. There are two main categories of igneous rocks:Intrusive – formed underground Extrusive – formed above ground
  • 23.
  • 25.
  • 26. ← Obsidian Pumice ->
  • 27. Basalt – vesicular (with holes), dense, and thin-section
  • 28.
  • 32.
  • 34. Slate with Pyrite ↓ ↑ Slate (plain)
  • 35. Gneiss