1. Lecture 22 By thought and dint of hammering, Is the good work done whereof I sing, And a jollier crowd you´ll rarely find, than the men who chip on earth´s old rind, And often wear a patched behind, By thought and dint of hammering. - Andrew C. Lawson Structural Geology Webpage for course (daytime) Webpage for course (nighttime)

2. Map quiz 25 (2) 24 (2) 23 22 (2) 21 (6) 20 (3) 19 (5) 18 (2) 17 (2) 16 (2) 15 14 (2) 12 (2) 10 8

3. As we learned from James Hutton: Originally strata are: horizontal layers younger beds above older ones

4. Fig. 18-4, pg. 420

5. Sedimentary rocks are deposited in Flat-lying layers subsequently FOLDED FAULTED REMOVED THROUGH EROSION

6. Folds anticlinesyncline

7. Fig. 18-8 A-B

8. anticlines and synclines Fig. 17-3 A Fig. 17-3 B

9. How to identify eroded folds Relative age

10. Kinds of mountains Fault Block Fold and Thrust Volcanic

11. Faults Hanging wall Foot wall

12. Faults Hanging wall Foot wall Hanging wall Foot wall

13. Normal fault Reverse fault Fig. 17-9 A Fig. 17-9 B

14. How to identify type of fault Relative age

15. Thrust faults Fig. 17-9 B

16. Kinds of mountains Fault Block Fold and Thrust Volcanic

17. weathering Fig. 8 B-C

18. Fig. 8 C-D Erosional unconformity

20. Folds anticlinesyncline