1. Earth’s major plates Note: Boundaries rarely correspond to the contact between oceans and continents!

2. Implied rates of plate divergence, convergence and strike-slip motion

3. Rayleigh number = Buoyancy Viscous drag X Momentum diffusivity Thermal diffusivity accelerationThermal expansion Kinematic viscosityThermal diffusivity Length scale Temperature contrast

4. A numerical model of whole-mantle convection in a 2-D earth

6. Types of plate boundaries

8. Relation between igneous activity and plate boundaries

9. Starting point: Continents and oceans are the pieces of an Eden broken up by the great flood:

10. 1: The earth is divided into continents and oceans Alfred Wegener proposes continental drift ca. 1912 Alfred Wegener, ca. 1920, in a weird hat.

11. 2: The continents look like pieces of a puzzle, and share elements of their geology.

12. 3: The distribution of fossil animals and plants re-enforces the tie-points between the continents

13. 4: The edges of the continents are locations of faulting and seismicity

14. 5: when continents rift apart, you find an ocean between them Rift Horst Graben

15. Put it all together, and see that the continents were once connected but have drifted apart by ‘sliding’ over or ‘plowing’ through the ocean floor Driving force: mystery, or centrifugal force, or both

16. Counter-arguments This is just stupid Any force strong enough to ‘push’ a continent over a bed of ocean floor would internally deform the continent instead

17. Counter-arguments Not all pieces of the continental puzzle really match

18. Counter-arguments Many continental margins don’t even fit geometrically

19. Counter-arguments Even if they fit, so what! Lots of ‘fits’ are possible just by chance

20. Breakthrough: Harry Hess and the exploration of the ocean floor Led to discovery that the ocean floor is the active part of the plate system, not the passive medium through which continents move. A ridge

21. A ridge and its transforms seen in plan view

22. Ahh, trenches

23. The real story with seismicity Wagener was only partially correct. The ring of fire is a locus of faulting, but there are other loci not expected if continents drift

24. And, the seismicity at the edges of the ring of fire don’t represent continents sliding over oceans; they are places where ocean floor plunges into the deep earth interior. Benioff-Wadati zones

25. Centered on most great belts of seismicity, and is rare elsewhere Active Volcanism

26. 1600: Recognition that earth has a magnetic field; supposed to be like a ‘lodestone’ (magnetite with a permanent magnetic field) 1919: Larmor proposes it is actually a dynamo 1946: Elsasser explains field as consequence of convection of induced electric currents in liquid outer core

27. Geodynamo Ohmic decay would dissipate earth’s field, if static, in ~20,000 years Therefore, must be sustained by some dissipative process (convection) Fundamental cause of magnetism is induction in a convecting, conducting medium – electrically conductive medium – convection in response to density gradients in that medium – maintenance of density gradients by heat generation/exchange and/or chemical differentiation ~80% dipole; rest other modes Varies in intensity and orientation and relative strength of various harmonic components with a wide range of t constants

28. Numerical model of ‘tangled’ magnetic field lines in core

29. Terrestrial Magnetism Inclination… …and declination

30. Intensity (in mysterious units — 10,000  ’s) Map of inclination

31. Preservation in rocks of the orientation of the magnetic field

32. spin of unpaired electrons in the Fe +2 and Fe +3 sub-lattices can order at low temperature. These oppose each other, but are unequal, leading to a net magnetic moment Fe +3 only Fe +3 and Fe +2 Ferrimagnetism in magnetite

33. Variation through time of the apparent location of the north magnetic pole, based on records from North American rocks

34. Phanerozoic records of magnetic polar wander from Europe and North America disagree…unless they have moved relative to each other (or, the shape of the Earth’s magnetic field has varied) Interesting, but all it really does is support and ‘flesh out’ Wegener’s view of ‘continental drift’.

35. Much more important is an incredibly subtle detail to the fine structure of the modern magnetic field…

36. A closer look… Measured Anomaly (I.e., relative to long-wavelength field)

37. The anomalies represent positive and negative interference from magnetic rocks in the crust A magnetic ‘reversal’ occurs between these two times

38. How do we know? We’ve seen them appear after volcanic eruptions on the sea floor.

39. Some real examples

40. Calibrating the ocean floor’s ‘strip-chart recorder’ 1: Collecting samples with the Glomar Challenger

41. K-Ar dating 40 K 40 Ca 40 Ar 88.8 %11.2 % e - capture; e = 0.581x10 -10 yr -11 e - emission;  = 4.982x10 -10 yr -1 40 Ar = e / 40 K(e t -1) + 40 Ar 0 = e +  = 5.543x10 -10 yr -1 0.01167 % of natural K

42. Some ‘closure temperatures’ w/r to K/Ar dating: Amphibole: 500 to 700 ˚C Biotite: 300 to 400 ˚C K-feldspar: 200-250 ˚C

43. Use in dating magnetic reversals

44. Maps of magnetic ‘stripes’

45. Sometimes it’s fun to pretend that our record of the seafloor’s magnetic stripes is complete: