1. Plate Tectonics Evolution of the Earth Free powerpoints at http://www.worldofteaching.comhttp://www.worldofteaching.com

2. How do we know anything about the Earth Interior structure Volcanoes and hotspots Earthquakes Tectonic plates Tectonic motion Reconstruction of the Earth’s history Interior structure Volcanoes and hotspots Earthquakes Tectonic plates Tectonic motion Reconstruction of the Earth’s history

3. Interior

5. What’s in the Earth’s Layers: Crust: is made up of Silicates Mantle: -Lithosphere: upper part of the mantle and the earht’s crust made up cooler-rigid rock. -Asthenosphere: middle part of mantle made up softer weaker rock that can flow slowly. -Mesosphere: stiffer rock that goes to the core. Core: -Outer core: liquid metal and very hot! -Inner core: solid metal and very high pressure!

6. Volcanoes Volcanoes are the result of hot spots within the crust or mantle of the earth. The hot, liquid rock will break through weak spots in the surface and form volcanoes or flood basalts. Many volcanoes do not release lava, instead they spit ash and small bits of lava called lapilli. Some eruptions are quiet with very fluid (low viscosity (flow) ) lava flows while others are explosive

7. Volcanoes Quiet lava flows

8. Volcanoes Mt. St. Helen before the explosive eruption

9. Volcanoes

10. Time lapse of the eruption

11. Volcanoes Mt. St. Helen after the eruption

12. Volcanoes Mt. St. Helens begins the rebuilding process

13. Volcanoes

15. Shield Volcanoes: produce when low-vicosity lava makes a wide flat volcano.

16. Flood basalts: When volcanic eruptions coats a thick layer of magma over the surface of the earth.

17. Volcanoes

18. Flood basalts Basalt is a type of rock that is produced from the mantle Basalt is a type of rock that is produced from the mantle

19. Magma is always moving in the earth’s mantle due to Convection: Hot materials rising and cool materials sinking. This causes the plates to 1) move apart (Divergent Boundaries) or 2) move together (Convergent Boundaries) and even 3) past one another (Transform Boundaries.)

20. Because Plates move they cause the magma to be released through volcanoes of various types and sizes.

21. Volcano locations: Why at these locations?

22. The reason volcanoes occur at specific locations: 1. Plate Tectonics Move at a Subduction (Convergent) Zone:

23. Convergent Zones: Volcanoes

24. The reason volcanoes occur at specific locations: 2. At Divergent Zones:

25. The reason volcanoes occur at specific locations: 3. Magma moves to the surface of the earth near a weak spot and can activate a magma chamber http://sio.ucsd.edu/volcano/about/magma.html 4. This can happen over a HOTSPOT. The Hawaiian Islands have formed because a plate moved over a hotspot.

26. Different Forms of Energy In the Earth Mechanical Energy: Energy due to motion Heat energy: energy due to heat Potential energy: energy that is built up but not yet released Kinetic Energy: energy that is occurring (in motion)

27. What types of energy are taking place to have a volcano? Mechanical Energy: –Magma moves from the interior earth up to a weak portion in the earth’s crust. –Magma also moves out from the volcano. –Ash and rock can also move out from a volcano like in a pyroclastic flow. Heat Energy –The earth’s core has large amounts of heat that escape at the earth’s surface through a volcano Draw how a volcano works by using words to describe the process such as: magma, crust, mantle, mechanical energy, heat energy

28. Earthquakes Earthquakes are a result of motion within the earth. This only occurs where the earth is solid and therefore can only occur within about 100 miles of the surface Earthquakes provide the best evidence regarding the interior structure of the Earth.

29. Earthquakes

33. Types of seismic wave There are two types of seismic wave, namely, 'body wave' and 'surface wave' Body waves travel through the interior of the Earth. They follow raypaths bent by the varying density and stiffness of the Earth's interior. density Surface waves are similar to water waves and travel just under the Earth's surface. They travel more slowly than body waves. Because of their low frequency, long duration, and large amplitude, they can be the most destructive type of seismic wave.Surface waves

34. Body Waves and Surface waves fall under two categories: 1)P-Waves: occurs when fault moves past each other horizontally, cause a compressed wave. 2)S-Waves: occurs when faults move vertically, causes a wavy wave.

35. Both Body Waves and Surface Waves will differ in both S & P Waves:

36. Seismograph: Measures movement in the earth.

37. Finding an Earthquake’s Epicenter

39. Earthquakes Tidal waves or Tsunamis result when a large section of the sea floor suddenly moves and therefore displaces a massive amount of water.

40. Tidal waves or Tsunamis result when the low amplitude long wavelength waves reach the shallow shoreline and begin to feel the bottom of the sea floor. This Shortens the wavelength and increase the amplitude (height).

41. Earthquakes Location of worldwide earthquakes

42. Earthquakes Earthquakes by depth. Notice that the deep earthquakes occur only at subduction zones.

43. Based on Motion It turns out that the upper section of the mantle is adhered (stuck to the underside side of the crust to form what we call tectonic plates

44. Tectonic Plates

45. Today plate boundaries are determined by examining the location of volcanoes and earthquakes. Volcanoes result from the friction (heat) of the plates motion. Earthquakes occur where plate rub against one another

46. Tectonic Plates Our first evidence of tectonic motion is based on similar fossils and rock types on opposing sides of the ocean

47. Tectonic Plates

48. Earthquakes

49. Tectonic Plates Volcanoes

50. Tectonic Plates

53. Another source of evidence is based on seafloor ages which get younger as we approach sea floor ridges

54. Tectonic Plates Our final piece of evidence is the magnetic record of the ocean floor. This shows the pattern of reversal and we find a near perfect mirror image on opposing sides of the ridge

55. Tectonic Plates

58. Composition vs. Motion We can look at the interior of the Earth based on the composition of the rocks or based on the movement

59. Based on Composition Crust – solid, relatively low density silicate rock Mantle – Semi fluid, denser, mafic (iron and magnesium bearing) rocks Core – Liquid then solid iron and nickel with traces of heavier elements

60. Plate Types Oceanic plates: basalt –Dark (black) and dense rock type composed of silicates, iron and magnesium Continental plates – granite and andesite –Light colored (pink, white and gray) and low density rock type composed almost entirely of silicates.

61. Plate Boundaries Convergent – plates move toward one another Divergent – plates move away from each other Transform – plate moves sideways from each other

62. Faults occur at these Plate boundaries, where land masses move. These faults when moved release energy in the form of an earthquake. There are 3 different faults: 1. Normal Fault: as stress is pulled away on the plates, one land mass slips down. (Divergent Plate boundary)

63. 2. Reverse Fault: as two plates come together one land mass jets up above the other making a hanging wall. (Convergent Plate Boundary) 3. Transverse Fault: occurs as two plates slide past one another. (Transform plate boundary)

64. Plate Boundaries

66. Convergent Plates

69. The only subduction zone in the Atlantic The only subduction zone in the Atlantic

70. Convergent Plates Black arrows show subduction zones and the direction of plate movement

71. Convergent Plates Looking at the depth of earthquakes shows that angle that the plate is being subducted

72. Divergent Plates

76. Transform Plates

77. San Andreas Fault

78. Mid-Plate Hotspots

82. Why do the Plates Move?

83. No single idea explains everything but we can identify several forces that contribute to the movement of the plates. –Slab pull The sinking of the cooled dense oceanic plates pulls on the rest of the plate –Ridge rises The material deposited on the top of the ridge slides downs from the rise pushing on the plate –Convection Movement within the mantle could be part of the driving force behind the motion of the plates.

84. The Big Picture

85. Pangea What is Pangaea? Pangaea was a super continent at one time. Scientists use the similarity of rock types and fossil types that date to the same age to support their theory that the continents were connected to form a super continent. The map below give just one example of areas on different continents that show the same fossils and rock types.

86. Pangea

88. The break up of Pangea

89. Where are we going? We appear to be headed for another super continent as North America, South America, Asia and Australia converge in the ever shrinking Pacific Ocean