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58 Pages

13 Structural Geology

Course: GEOLOGY 100, Spring 2011
School: Rutgers
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Word Count: 365

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Alps Fig. The 11.00 Stephen Marshak Major Mountain Ranges Fig. 11.02 National Geophysical Data Center/NOAA Fig. 11.03ab Anorogenic W. W. Norton Orogenic Components of Deformation Fig. 11.04ab Evidence of Deformation Fig. 11.04cd Flat-lying strata of the Badlands Fig. 11.05a Stephen Marshak Tilted (dipping) strata in Arizona Fig. 11.05b Stephen Marshak Folding Fig. 11.05c Stephen Marshak...

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Alps Fig. The 11.00 Stephen Marshak Major Mountain Ranges Fig. 11.02 National Geophysical Data Center/NOAA Fig. 11.03ab Anorogenic W. W. Norton Orogenic Components of Deformation Fig. 11.04ab Evidence of Deformation Fig. 11.04cd Flat-lying strata of the Badlands Fig. 11.05a Stephen Marshak Tilted (dipping) strata in Arizona Fig. 11.05b Stephen Marshak Folding Fig. 11.05c Stephen Marshak Deformation illustrated Fig. 11.06ab W. W. Norton Other types of deformation Fig. 11.06cd W. W. Norton Fig. 11.07 W. W. Norton Shearing Fig. 11.08ab W. W. Norton Deformation types Joints in sandstone Fig. 11.08c Stephen Marshak Folded marble Fig. 11.08d Stephen Marshak Fig. 11.11ab W. W. Norton Dip and Strike Vertical joints Fig. 11.12b Stephen Marshak Fault Fig. 11.13b Stephen Marshak Fig. 11.14a W. W. Norton Fig. 11.14b W. W. Norton Fig. 11.14cd W. W. Norton Fig. 11.15ab Fault Scarp Fig. 11.15c Stephen Marshak Thrust faults Fig. 11.16 W. W. Norton Thrust-fault system Fig. 11.17a W. W. Norton Fig. 11.17b Normal fault system W. W. Norton Horst and Graben structure Fig. 11.18ab Fig. 11.19abc W. W. Norton Parts of a fold Fig. 11.19fg W. W. Norton Road-cut: anticline Fig. 11.20a Stephen 11.20b Stephen Marshak Road-cut: Syncline Fig. Marshak Asymmetrical folds Fig. 11.20d Stephen Marshak Folded strata Fig. 11.21ab W. W. Norton Plunging fold Fig. 11.21cde W. W. Norton Dome Basin Process of Folding 11_1.exe Causes of folding Fig. 11.23 W. W. Norton Development of foliation in a rock Fig. 11.24a W. W. Norton Fig. 11.24b W. W. Norton Fig. 11.24cd Schistosity develops during shear Fig. 11.24ef Structures developed in an orogeny Fig. 11.25 W. W. Norton Grand Tetons: 2 km of vertical relief Fig. 11.26 Stephen Marhsak Fig. 11.27 W. W. Norton Glacially carved peaks in Switzerland Fig. 11.28a Stephen Marshak Convergent-margin orogen (western US) Fig. 11.31a W. W. Norton Fig. 11.31b Collisional orogen: two continents collide Fault-block mountains: crustal thinning Fig. 11.33 W. W. Norton U.S. Topography Fig. 11.34 U.S. Geological Survey p.342-343a Original artwork by Gary Hincks India-Asia collision: Himalayas p.342-343b p.342-343c Original artwork by Gary Hincks Domes and basins of the Mid-continent Fig. 11.35a Fig. 11.35b W. W. Norton Evolution of the Appalachians Fig. 11.36abc NOAA Fig. 11.36a NOAA Fig. 11.36b NOAA Fig. 11.36c NOAA Fig. 11.37 W. W. Norton
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CHAPTER 8VALUATION OF INVENTORIES: A COST-BASIS APPROACHIFRS questions are available at the end of this chapter.TRUE-FALSE-ConceptualAnswerT F F F T T F T F T T F F T T F F T F TNo.1. 2. 3. 4. 5. 6. 7. 8. 9. 10. 11. 12. 13. 14. 15. 16. 17. 18. 19.
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CHAPTER 9INVENTORIES: ADDITIONAL VALUATION ISSUESIFRS questions are available at the end of this chapter.TRUE-FALSE-ConceptualAnswerT F F T F T T F F T F T F T F F T F T TNo.1. 2. 3. 4. 5. 6. 7. 8. 9. 10. 11. 12. 13. 14. 15. 16. 17. 18. 19. 20Desc
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CHAPTER 19ACCOUNTING FOR INCOME TAXESIFRS questions are available at the end of this chapter.TRUE-FALSE-ConceptualAnswerF F T T F T F T F T F T T F F T T T F FNo.1. 2. 3. 4. 5. 6. 7. 8. 9. 10. 11. 12. 13. 14. 15. 16. 17. 18. 19. 20.DescriptionTax
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CHAPTER 20ACCOUNTING FOR PENSIONS AND POSTRETIREMENT BENEFITSIFRS questions are available at the end of this chapter.TRUE-FALSE-ConceptualAnswerF T F T T F F T F T F F T F T F T F F TNo.1. 2. 3. 4. 5. 6. 7. 8. 9. 10. 11. 12. 13. 14. 15. 16. 17. 18.
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CHAPTER 22ACCOUNTING CHANGES AND ERROR ANALYSISTRUE-FALSE-ConceptualAnswerF T F T F T T T F T F F T F T T F F T TNo.1. 2. 3. 4. 5. 6. 7. 8. 9. 10. 11. 12. 13. 14. 15. 16. 17. 18. 19. 20.DescriptionChange in accounting estimate. Errors in financial
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