Rocks

  • A rock is a naturally formed consolidated material composed of grains of one or more minerals
  • Earth’s surface is extremely diverse in terms of rock makeup and types etc
  • Made up of one or more minerals/pieces of other rocks
  • They form through different geologic processes
  • Three types of rocks, Igneous, Sedimentary, Metamorphic, all defined by the process that creates them
  • The rock cycle shows how rocks are created and destroyed
    • Plate tectonics play an important role in the rock cycle
    • Sediments are transported, buried and lithified, forming sedimentary rocks
    • Sedimentary and igneous rocks are altered forming metamorphic rocks
    • Earth’s internal heat and pressure melts material, producing igneous rocks
    • Plate Tectonics and the rock cycle
    • Uplift (surface exposure) happens due to tectonics. Mostly happens at convergent boundaries
    • Space for sediments is often created by tectonic motions, at divergent boundaries
    • Metamorphism often occurs at convergent boundaries. It can alter any type of rock

Igneous Rocks

Sedimentary Rocks

Metamorphic Rocks

Minerals

  • minerals are naturally occurring, inorganic, crystalline solids
    • they have specific chemical composition and distinctive physical properties
  • Rocks are composed of one or more minerals
  • Minerals have 5 characteristics
    • Solid
    • Naturally ocurring
    • Inorganic
    • Ordered internal structure (crystalline)
      • Orderly arrangement of atoms in a repeating pattern
      • The internal structure influences the external form
    • Specific chemical composition
  • About 4,000 minerals have been found so far
  • Major mineral groups
    • Silicates (SiO)
      • Make up most of our crust so very important
      • These minerals are made up of Silica Tetrahedra. A silica atom surrounded by four Oxygen atoms
    • Carbonates (CaCO)
    • Halides (F, Br, Cl, I)
    • Oxides (O + metal)
    • Sulfides (S + metal)
    • Sulfates (S + O)
    • Native minerals (single elements)
  • Key Minerals are Quartz and Feldspar (both abundant at the surface) and Olivine and Pyroxene (both abundant in mantle)

Atoms, Elements, and Isotopes

  • Chemical elements make up matter
    • Atoms: nucleus (protons and neutrons) and electrons
  • Atomic Number
    • Number of protons (= # of electrons)
      • Determines the element
  • Atomic mass number
    • Number of protons + neutrons
  • Isotopes
    • Same element, different numbers of neutrons
    • Some isotopes are stable, some are unstable
      • Some unstable ones decay to a more stable one
  • Making a mineral involves the bonding of atoms
  • The type of bonding can affect a minerals strength and qualities (e.g. covalent vs ionic bonds)