OBJECTIVES
Chapter 10 - Crustal Deformation
1. Define "compressional stress" and list the structures produced from them.
2. Define "tensional stress" and list the structures produced from them.
3. Define the following:
confining pressure shear
brittle ductile
plastic deformation elastic deformation
4. Describe how increased pressure affects the volume and brittle-ductile properties of rock.
5. Describe how the following terms relate to rock failure and explain the elastic-strain hypothesis:
a. yield point c. strain
b. stress d. primary, secondary, and tertiary creep
6. Define strike and dip.
7. Differentiate between the following kinds of folds or terms:
Monocline Plunging anticline
anticline Plunging syncline
syncline recumbent fold
8. Differentiate between a structural basin and dome on the basis of dip/strike and distribution of age of rock.
9. How is a structural basin and dome different from a hill and a valley?
10. Give the features of and differentiate between dip-slip faults and define:
reverse fault oblique-slip faults
thrust fault normal fault
11. Define the following:
fault block mountain. graben
horst fault scarp
12. Define "strike-slip" fault and differentiate between:
left lateral right lateral
13. Cite examples of crustal uplift.
14. Describe the concept of mountains with "roots" and be able to apply the principle of isostancy to mountains with roots.
15.
Describe all forms of mountain building resulting from convergent boundaries
and give modern examples of each and explain how they differ from each other
based on the structures and mountains that form
Oceanic to oceanic convergence (this is a trick…there are no true mountains formed at this setting…only islands)
Oceanic to continental convergence
Continental to continental convergence
16.
Describe the mechanism of fault-block mountain building and discuss the
possible causes of
spreading".
17. Describe the mechanism of post orogenic uplift and give an example of the process ongoing today.
18.
Explain the concept of accreted terranes and how they
dominated the formation of