Chapter 10: Deformation (Strain) and Mountains Flashcards
Dip
Angle and direction of inclination of a surface
-Perpendicular to strike
Strike
The direction of a line formed by the intersection of an inclined surface and a horizontal plane
-Perpendicular to dip
Stress
Force applied; source is mantle convection
Compression –>
Shear –>
<–
Strain
Deformation caused by stress
-Depends on type of material (brittle or ductile), Amount of stress (rate), and location (depth: pressure and temp)
Brittle Materials
Elastic strain and Fracture
Ductile Materials
Plastic Strain (flow) results in perm change of shape (folding)
- Slower stress, greater confining pressure, higher temp, and greater water content makes this more likely
- Plastic limit is when fracture occurs
Folds
Result from compression and plastic strain
Anticline
Folds where the oldest rocks are in the center at ground surface and all layers dip away from axis
Syncline
Folds where the youngest rocks are in the center at ground surface and all layers dip toward axis
Faults
Results from rupture and slip
Dip-slip faults
Vertical movement
- Reverse: compressive stress, H up, F down
- Thrust fault: low angle (<45 degrees) reverse fault
- Normal: tensile stress, H down, F up
Strike-slip fault
Horizontal movement; transform faults, shear stress
- Right lateral
- Left lateral
Mountain Building
Orogenisis at convergent plate boundaries (growth of continents)