Folding and Faulting (Grade 10 NSC Matric Geography): Flashcards

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Faulting
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Fault (geology)

Crack in rocks where movement occurred along the break

Fault plane

Surface where rock fracture occurs

Three types of stress forces on rocks

Tension (stretch), compression (squeeze), sideways sliding

Normal fault formation

Tension pulls rocks apart; one block drops down

Reverse fault formation

Compression squeezes rocks; one block pushes upward

Lateral/strike-slip fault movement

Horizontal - blocks slide past each other sideways

Transform fault characteristics

At right angles to plate boundaries; extend 100s of km

Rift valley formation

Tension causes land blocks to drop down between parallel faults

East African Rift Valley dimensions

Approx. 6000 km long, 20-60 km wide

Block mountain formation

Compression pushes crust blocks upward next to rift valleys

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