1. Chapter 22 ISCI 2001 Structure of the Earth Tectonics

2. Structure of the Earth

3. Crust (1). Thin, brittle Oceanic Basalt rock (dark); greater density Continental Granitic rock (lighter); less dense Less dense than mantle Floats

4. Mantle (1). Most of the volume (82%) and mass (65%) – Thickest layer (2). Rich in Si and O – Contains Fe, Mg, Ca (causes increased density) Density increased by weight of crust also (3). Hotter than crust – High pressure Caused by radio active decay of elements Flow of heat from core (4). Regions – Upper Mantle – Lithosphere Stiff, cool – similar to crust (forms one layer together) – Asthenosphere Solid, plastic (solid flow) (5). Upper Mantle – Solid and rigid – Plastic but not as much as upper mantle

5. Core Consist of: Metallic Fe 2x dense as mantle (2). Inner Core Solid 4000 to 7000 C Radioactive elements Earth development; matter hitting the surface Core sinking to the center (3). Outer Core Flows due to less pressure Rotation of Earth stirs up core material Produces magnetic field (flowing electrical charge)

6. Plate Tectonics (1). Continents sit atop of tectonic ‘plates’ What are the plates made of? What is a continent? (2). Plates Consist of mantle and the crust (lithosphere) Plates move atop the asthenosphere (plastic) Continents move because they are embedded into the plates (3). Plate boundaries and continents Continents and plates do not have the same boundaries (overlapping) Figure 22.18 A lot of action occurs at the plate boundaries!

7. Plates

8. How were the Plates Discovered? (1). Alfred Wegener Proposed the theory of “Continental Drift” Continents are in motion; drifting over geologic time Pangea (figure 22.8) Same fossils found in several different continents Matching rocks on both sides of Atlantic Ocean (2). Evidence for CD Seafloor Spreading Magnetic Stripes

9. Pangea

10. Evidence for Continental Drift – Seafloor Spreading (1). Magma flows out of breaks in lithosphere New lithosphere is formed and old lithosphere will be recycled back in trenches (22.16) Mid-ocean ridge Pushes the continents in specific directions

11. Evidence – Magnetic Stripes (1). Lava contains Fe and magnetite (Fe and O) Crystals are magnetic – line up with the magnetic field of the Earth Crystals point North and south / cool and freeze and become locked in Contains a record of the history of the magnetic field of the Earth Gives a striped, bar pattern (22.17) Alternates normal (today’s field) and reversed field from years ago. Runs along the spreading seafloor

12. How do the Plates Move? (1). As magma is heated deep in the Earth it moves upward via convection currents (22.21) Hot rocks from lower mantle move upward cool in the upper mantle and return Hit the lithosphere and can crack it – seafloor spreading Plates move atop ‘convection cells’

13. ISCI 2001 Chapters 22-24 Plate Tectonics

14. Plate Activities – Divergent Plate Boundaries (1). Plates may ‘diverge’ Plates move apart Lava fills spaces in between (2). What types of structures are produced? Volcanic mountains Rift valleys (3). Examples Mid-Atlantic Ridge Great Rift Valley (Africa near Nairobi Kenya)

15. Seafloor Spreading Rift Valley in Kenya

16. Mid-Atlantic Ridge

17. Convergent Boundaries (1). When two plates collide One plate usually subducts Most dense or oldest plates

18. Oceanic – Oceanic Trench formation (Marianas Trench) 11,000 m or 7.0 miles deep Pacific and Phillipine Plates collide Formation of volcanic islands or arcs Subduction plate mantle rock melts comes to the surface and cools

19. Marianas Trench

20. Oceanic – Continental Oceanic basaltic plate (more dense) subducts under granitic continental plate Mantle rock melts, magma rises and cools forms island chains Volcanic Arcs (Peru)

21. Oceanic – Continental The convergence of the Nazca and South American Plates has deformed and pushed up limestone strata to form the towering peaks of the Andes, as seen here in the Pachapaqui mining area in Peru.

22. Continental – Continental Massive plate collisions (both granitic) No subduction, why? Both have same density Massive mountains are formed Himalayas

23. Continental – Continental

24. Transform Plate Boundaries (1). ‘Sliding Plate’ Boundaries Slipping of plates causes ‘faults’ (2). Slipping causes plate movements Boundaries move in opposite directions against each other (3). Where are they normally found? Mostly ocean basins Continental plate: San Andreas Fault

25. San Andreas Fault

26. Faults Parts of a Fault Normal Faults Dip-slip Reverse Faults Strike-Slip

27. Types of Faults (1). Dip-Slip (See figure 24.5) Hanging wall and vertical wall move vertically along the fault plane Movement is vertical (2). Strike-Slip Movement is horizontal San Andreas Fault motion (3). Oblique Move horizontally and vertically

28. Slip-Dip Conjugate Normal faults, Canyonlands National Park, Utah

29. Fault Types

30. Folding (1). Bending in Rock layers Caused by compression (2). Results Anticlines or synclines

31. (1). Folded Mountains During formation continental crust thickens and wrinkles into vertical folds from compression Appalachians, Rockies and Himalayas (2). Unwarped Domed shaped Single anticline (crust is heaved upwards; no folds produced) Adirondack mountains NY (3). Fault-Block Land is ‘uplifted’, stretched and elongated Very steep profile Tetons (Wyoming); Sierra Nevada (California)

32. Mountain Formation Folded Mountain – Antarctica

33. Mountain Formation Adirondack Mountains – unwarped

34. Mountain Formation- (Fault-Block)

35. (1). Earthquakes Transform faults Compression and tension caused by stress of plate movements --  Slipping Focus location Rock is snapped or broken releasing ‘elastic’ energy (2). Types Intraplate (10%) Away from plate boundaries New Madrid, Missouri Interplate (90%) Plate boundaries Transform plates (mild Eqs) Subduction zones (strong)

36. Earthquakes

37. Subduction Zones – Ring of Fire! 80% of all interplate EQs occur here

38. Powerful Interplate EQs and Tsunamis (1). Coast of Sumatra Indian and Burma Plate collision Megathrust quake 100 billion tons of TNT (2). Production of a Tsunami Quake took place in the Indian ocean As subduction occurred The seafloor bent as the other plate sank Stress caused rock to snap and thrust upwards Force caused water to creat large wave 30m +/- above sea level

39. Earthquakes – San Francisco 1906

40. Magnitude of Earthquakes –Richter Scale (1). Logarithmic scale Each point represents a 10-fold increase in quake shaking strength Measures shaking Also indicates 30 fold increase in energy output 1 thru 10 Examples 1906 San Francisco (8.2) Sumatran 2004 (9.0)

41. Richter Scale

42. Tsunami

43. Sumatra EQ and Tsunami 184,000 People died

44. Surface and Ground Water

45. Watershed

46. Ocean Floor

47. Surface Water – Surface Processes

48. Glaciers