• COASTAL FEATURES OF EROSION
    PHYSICAL GEOGRAPHY

    COASTAL FEATURES OF EROSION

    1) Capes and bays: On exposed coasts, the continual action of waves on rocks of varying resistance causes the coastline to be eroded irregularly. This is particularly pronounced where hard rocks, e.g. granites and limestones, occur in alternate bands with…

  • THE MECHANISM OF MARINE EROSION
    PHYSICAL GEOGRAPHY

    THE MECHANISM OF MARINE EROSION

    The most powerful agents of marine erosion are waves. Their origin is due to the sweeping of winds over the water surface, which sets a series of undulating swells surging forward. These become higher and swifter. A normal wave in…

  • LANDFORMS OF WIND EROSION IN DESERTS
    PHYSICAL GEOGRAPHY

    LANDFORMS OF WIND EROSION IN DESERTS

    In the combined processes of abrasion, deflation and attrition, a wealth of characteristic desert landforms emerge. 1) Rock pedestals or mushroom rocks: The sand-blasting effect of winds against any projecting rock masses wear back the softer layer so that an…

  • THE MECHANISM OF ARID EROSION
    PHYSICAL GEOGRAPHY

    THE MECHANISM OF ARID EROSION

    Arid landforms are as a result of many combined factors, one reacting upon the other. Insufficient rainfall, often less than 127 mm (5 inches), coming at most irregular periods, coupled with very high temperatures (31°C/87°F, is the average) and a…

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