Week 4, Chpt 5 Flashcards
Horizontal compression drives
collision.
Horizontal tension drives
crustal rifting.
Stress is when
pressure is equal on all sides.
3 Types of Plate Boundaries
Dip-slip faults
Strike-slip faults
Oblique-slip faults
Anticlines
A shaped folds
U shaped folds
Synclines
Monoclines
Folds at a mountain range edge
Joints
Cracks in the rocks, they run parallel to each other. These are not faults.
When a joint fills up with mineral it is called a
vein.
How are mountains built? (4 ways)
Continental collision
Convergent boundaries
Continental rifting
Delamination
Isostacy
Surface elevation is a balance between forces of gravitational attraction and buoyancy. The crust is floating on the mantle.
Tearing the continent apart, the continent gets thinner.
Continental rifting
Delamination
As the mantle gets cold the lithosphere gets thicker and denser. The mantle underneath the continent breaks off and sinks, causing the crust above it to rise.
Stress (equation)
Force divided by area.
Strain
Deformation expressed as a fraction of original body geometry.