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33 Cards in this Set

  • Front
  • Back

Brittle

Breaks off after stress removed. (low temp+ pressure)





Ductile

Bent. (High temp + pressure)





Brittle Behavior

Faults and Joints (Near the surface)



Ductile Behavior

Folds

Anticline

Upward arching fold. "A"



Syncline

Downward arching fold

Hingline

Axis of a fold,

Axial Plane

Plane through hinglines of a fold. Divides fold into two limbs.

Dome

Bed dips away from central point. Oldest formation in center. (anticline)

Basins

Bed dips toward central point, oldest formation in center. (anticline)

Joints

Fractures where displacement has not occurred.

Fault

Fractures where displacement has occurred.

Dip-Slip

Movement parallel (vertical) to the dip of the fault plane.

Strike-Slip

Horizontal and parallel to the strike of the fault plane.

Oblique Slip

Movement with both vertical and horizontal components.

Normal Fault

Hanging wall block has moved down relative to footwall block due to tensional stress. (Divergent)

Reversed Fault

Footwall moves up relative to hangingwall (Divergent)

Thrust Fault

Reverse fault with dip angles less than 30 degrees horizontal

Graben

Fault block bounded by normal faults that drop down. ___ ___


` \____/

Horst

Opposite of Graben


____


___/ \___



Reverse Fault

Convergent, compression

Normal Fault

Divergent, tension

Strike-Slip

Transform, shear

Elastic Rebound Theory

Earthquakes are a sudden release of strain stored in rocks that bend until they break.

Focus (Hypocenter)

Where the slip initiates. (true location of earthquake)

Epicenter

Surface directly above focus.

Body Waves

Travel through Earth

P-waves

Compressional, travel through rock faster, magma slower

S-waves

Shear waves, travel through solids only

Love Waves

Horizontal shift of Earth during earthquakes

Rayleigh Waves

Surface waves that travel as ripples

Mercalli Intensity Scale

No mathematical scale

Richter Magnitude

based on greatest amplitude of earthquake