Earthquakes2
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Earthquakes2

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    Earthquakes2 Earthquakes2 Presentation Transcript

    • FAULTS Faul
    • FAULTS A fault is a planar fracture or discontinuity in a volume of rock, across which there has been significant displacement along the fractures as a result of earth movement.
    • FAULTS (DIPSLIP) A Normal Fault create space. Two blocks of crust pull apart, extending the crust.
    • FAULTS (DIPSLIP) Hanging Wall Footwall A Normal Fault create space. Two blocks of crust pull apart, extending the crust.
    • FAULTS (DIPSLIP) Reverse faults, also called thrust faults, squeeze the crust, pushing two blocks of crust on top of each other.
    • FAULTS (DIPSLIP) Reverse faults, also Hanging Wall Footwall called thrust faults, squeeze the crust, pushing two blocks of crust on top of each other.
    • FAULTS (DIPSLIP) Strike-slip faults indicate rocks are sliding past each other, with little to no vertical movement.
    • FAULTS (DIPSLIP) Top View Strike-slip faults indicate rocks are sliding past each other, with little to no vertical movement.
    • FAULTS Strike-slip faults indicate rocks are sliding past each other, with little to no vertical movement.
    • FAULTS Strike-slip faults indicate rocks are sliding past each other, with little to no vertical movement.
    • FAULTS system in the Philippines LAOAG CITY
    • FAULTS system in the Philippines MARIKINA VALLEY FAULT SYSTEM
    • FAULTS system in the Philippines Near BORONGAN
    • FAULTS system in the Philippines GENERAL SANTOS CITY