Geography: Landforms and Processes

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Study Notes

Mountain Formation

  • Types of Mountain Formation:
    • Volcanic: formed by volcanic activity, e.g., shield volcanoes
    • Fold: formed by folding of Earth's crust, e.g., Himalayas
    • Block: formed by faulting, e.g., Sierra Nevada
  • Mountain Building Processes:
    • Plate convergence: collision of tectonic plates
    • Uplift: vertical movement of Earth's surface
    • Volcanic activity: eruption of magma and lava

Volcanic Landforms

  • Types of Volcanic Landforms:
    • Shield volcanoes: gently sloping, broad volcanoes
    • Stratovolcanoes: tall, conical volcanoes
    • Calderas: large depressions formed by volcanic collapse
  • Volcanic Features:
    • Craters: depressions at the volcano's summit
    • Lava flows: streams of molten rock
    • Volcanic ash: fine particles ejected during eruptions

Desert Landscapes

  • Desert Features:
    • Dunes: ridges of sand formed by wind
    • Oases: isolated areas of vegetation in deserts
    • Playas: dry lake beds
  • Desert Formation Processes:
    • Wind erosion: removal of rock and soil by wind
    • Deflation: removal of loose sediment by wind
    • Deposition: accumulation of sediment in a new location

Plate Tectonics

  • Theory of Plate Tectonics:
    • Earth's lithosphere is divided into large plates
    • Plates move relative to each other, creating and destroying landforms
  • Plate Boundaries:
    • Divergent: plates moving apart, e.g., mid-ocean ridges
    • Convergent: plates moving together, e.g., subduction zones
    • Transform: plates sliding past each other, e.g., fault lines

Coastal Features

  • Types of Coastal Features:
    • Headlands: rocky areas that jut out into the sea
    • Bays: areas of coastline indented by the sea
    • Deltas: areas of sediment deposited at a river mouth
  • Coastal Processes:
    • Erosion: removal of rock and soil by the sea
    • Deposition: accumulation of sediment along the coast
    • Longshore drift: movement of sediment along the coast by currents

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