earthquakes2

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FAULTS Fau lt

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Page 1: Earthquakes2

FAULTS

Fault

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FAULTSA 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.

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FAULTS (DIP-SLIP)

A Normal Fault create space. Two blocks of crust pull apart, extending

the crust.

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FAULTS (DIP-SLIP)

A Normal Fault create space. Two blocks of crust pull apart, extending

the crust.Footwall

Hanging Wall

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Reverse faults, also called thrust

faults, squeeze the crust, pushing two blocks of crust on top of each other. 

FAULTS (DIP-SLIP)

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Footwall

Hanging WallReverse faults, also called thrust

faults, squeeze the crust, pushing two blocks of crust on top of each other. 

FAULTS (DIP-SLIP)

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Strike-slip faults indicate rocks are sliding past each other, with little

to no vertical movement.

FAULTS (DIP-SLIP)

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Strike-slip faults indicate rocks are sliding past each other, with little

to no vertical movement.

FAULTS (DIP-SLIP)

Top View

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FAULTS

Strike-slip faults indicate rocks are sliding past each other, with little

to no vertical movement.

Page 10: Earthquakes2

FAULTS

Strike-slip faults indicate rocks are sliding past each other, with little

to no vertical movement.

Page 11: Earthquakes2

LAOAG CITY

FAULTS system in the Philippines

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FAULTS system in the Philippines

MARIKINA VALLEY FAULT

SYSTEM

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FAULTS system in the Philippines

Near BORONGAN

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FAULTS system in the Philippines

GENERAL SANTOS

CITY