1. Plate Tectonics

2. Earth’s Interior

3. Alfred Wegener (1880-1930) German astronomer/meteorologist Worked in Greenland on polar air circulation Died on expedition in 1930 Proposed Continental Drift in 1912 German astronomer/meteorologist Worked in Greenland on polar air circulation Died on expedition in 1930 Proposed Continental Drift in 1912

4. Theory of Continental Drift -Earth’s continents had once been joined as a single landmass Pangaea “all lands” - Ancient landmass made up of all continents forming a supercontinent. - Began to break apart about 200 million years ago (mya) Continental Drift

6. Pangaea Ultima?

7. Evidence from Rock Formations Rock formations (ex. mountain ranges) fractured as the continents separated. Same rocks are found in the Appalachians and also in Greenland and Europe. Rock formations (ex. mountain ranges) fractured as the continents separated. Same rocks are found in the Appalachians and also in Greenland and Europe.

8. Evidence from Fossils Wegener found similar fossils of different land animals and plants on separated continents.

9. Ancient Climatic Evidence Sedimentary Rock Coal Coal forms from dead swamp plants. Coal was found in Antarctica, therefore Antarctica must have been closer to the equator at one time.

10. Ancient Climatic Evidence Cont. Glacial Deposits -290 mya glacial deposits found in Africa, India, Australia, and South America. -These continents were once located on the South Pole.

11. Continental Drift was rejected. People rejected the hypothesis because: 1- they believed continents and ocean basins were permanent, fixed features of Earth’s surface 2- Wegener could not explain what forces could cause a continent to move without shattering People rejected the hypothesis because: 1- they believed continents and ocean basins were permanent, fixed features of Earth’s surface 2- Wegener could not explain what forces could cause a continent to move without shattering

12. Sea-Floor Spreading

13. Isochron Map a line map that connects points of the same age. Check this out on Google EARTH.Google EARTH a line map that connects points of the same age. Check this out on Google EARTH.Google EARTH

14. Theory of Plate Tectonics Evidence 1. Rock Age Young Rocks – near ocean ridges. Older Rocks – near deep-sea trenches Ridges – the age of the oceanic crust increases with distance from a ridge. Seafloor Age – oldest part = 180 million years old. Oldest Continental crust = 3.8 billion years old. 1. Rock Age Young Rocks – near ocean ridges. Older Rocks – near deep-sea trenches Ridges – the age of the oceanic crust increases with distance from a ridge. Seafloor Age – oldest part = 180 million years old. Oldest Continental crust = 3.8 billion years old.

15. Earth’s Magnetic Field Our magnetic field is called the magnetosphere. It stretches out through the atmosphere and acts as a protective barrier to deadly, high-energy solar radiation.

16. Movement of the liquid outer core of the Earth generates a strong magnetic field that surrounds the planet. This causes the Earth to act much like a large magnet, with the poles of the magnet located near the poles of the Earth.

17. Theory of Plate Tectonics Evidence. 1960s Technology: Magnetometer –makes a map from detecting small changes in magnetic fields. Geologists mapped volcanoes and earthquakes along plate boundaries. Sonar – used to map out the seafloor

18. Theory of Plate Tectonics Evidence 2. Paleomagnetism is the past formation of rocks containing iron-bearing minerals which provide a record of earth’s magnetic field. Basaltic rocks are found in the ocean crust and are rich in iron and when they cool the iron-bearing minerals orient parallel to Earth’s magnetic field. Lava 2. Paleomagnetism is the past formation of rocks containing iron-bearing minerals which provide a record of earth’s magnetic field. Basaltic rocks are found in the ocean crust and are rich in iron and when they cool the iron-bearing minerals orient parallel to Earth’s magnetic field. Lava

19. Magnetism & Paleomagnetism support sea-floor spreading and Theory of Plate Tectonics.

20. Geomagnetic Time Scale Magnetic Reversal Normal Polarity Reversed Polarity Magnetic Reversal Normal Polarity Reversed Polarity a change in Earth’s magnetic field. a magnetic field that has the same orientation as Earth’s present field a magnetic field that is opposite to the present field

21. Major plates of the world.

22. Mid-ocean Ridge – crust is formed.

23. Subduction Zone – crust is destroyed.

24. Slab-pull and Convection Currents cause plate motion.

25. Plate Boundaries Three Major Types Plate Boundaries Three Major Types 1.Convergent - places where tectonic plates interact with one another. plates come together. 2.Divergent 3.Transform plates move away from one another. plates move horizontally past one another

26. Divergent Boundary

27. Divergent - Iceland Rift

28. Convergent Oceanic- Continental Boundary

29. Oceanic-Continental Cascade Range

30. Convergent Oceanic- oceanic Boundary

31. Convergent Continent- Continent Boundary

32. Continental-Continental Himalayas

33. Transform Boundary

34. Transform – San Andreas Fault

35. Know this drawing!