glacial dating- visualizing in 3D Flashcards
1
Q
Why do rocks fold and fault?
A
- when rocks are subjected to stress and undergo strain they fold and fault
- there are different kinds oof stress including compressional, tensoinal, and shear
2
Q
How do rocks respond to stress?
A
- rocks respond in two ways:
- Elastic strain: deformed body recovers when stress is removed. Think elastic band. When the stress is beyond the elastic limit, permanent deformation is caused
- Plastic strain: bends but does not return to original shape. Rocks under increased temperature/pressure. For example, rocks in the mantle. Ex. glacial ice, asthenosphere
- brittle
3
Q
*How do rocks fold?
A
- folds or bends in layered rocks. caused by plastic strain
- depending on the stress, strain behaviour on the rock changes. Folds can become permanent after strain is removed: this can casued a fault
- types of folds: anticline, syncline, overturned, recumbent
4
Q
What are fractures and faults?
A
joints- rocks fractures, no displacement (not a fault)
faults- fractures along which movements has taken place. An active fault is classified as having movement within 11000 years
- Types of faults: normal, reverse, thrust, strike slip
5
Q
How does fault formation reflect the type of stress to which rocks are subjected?*****
A
- different types of faults are caused by different types of stress
6
Q
anticline
A
- upward arching fold
- synclines and anticlines often occur together
7
Q
syncline
A
- downward arching fold
- synclines and anticlines often occur together
8
Q
overturned fold
A
anticline goes over syncline due to lots of folding
9
Q
recumbent fold
A
- axial plane is at the axsis of orientation. straight lines in the horizion
- axial plane is essentially horizontal,
10
Q
compressional stress
A
- forces pushing together
- convergent boundaries have compressional stress
- ex. convergent plate margins
11
Q
tensional stress
A
- forces pulling apart
- ex. divergent plant margins
12
Q
shear stress
A
- parallel; opposing forces
- ex. transform plate margins
13
Q
normal fault
A
- hanging wall block moves downward relative to footwall block
- caused by tensional stress
- can produce a graben or horst
- ex. East african rift valley, or just a rift valley in general
14
Q
reverse fault
A
- hanging wall block moves upwards relative to footwall block
- causes by compressional stress
- often caused by compressional stress
15
Q
thrust fault
A
- reverse fault with very low angle fault (less than 45 degrees)
- causes by compressional stress