3. Earth is made of three layers The earth is layered similar to a hardboiled egg Shell is thin and hard Egg white is thick and softer Yolk is small and at the center Crust—thin and rigid Crust—thin and rigid Mantle—hot Mantle—hot Core—made of iron Core—made of iron Earth HardBoiled Egg

4. Lithosphere—upper mantle and crustLithosphere—upper mantle and crust Asthenosphere— hot upper part of mantleAsthenosphere— hot upper part of mantle Ocean crust— thinnest crust, very denseOcean crust— thinnest crust, very dense Continental crust— thickest crust, not as denseContinental crust— thickest crust, not as dense

5. Plate Tectonics The theory that explains the formation, movement and subduction of the earth’s plates. The plates are moving Earth’s lithosphere is broken into separate sections called plates. Edges of plates meets at lines called plate boundaries. The theory that states:

6. Present Day Tectonic Plates Plate Boundary Fault

7. Evidence for Plate Tectonics Mid-Ocean Ridges Age of the ocean crust Ocean Trenches Magnetic stripes on the sea floor

8. Scientists started mapping the ocean floor in the 1950’s, At the center of the ocean, They found huge underwater mountain ranges, This was a surprise because they expected the ocean to be flat in the middle of the ocean Scientists called the huge underwater mountain ranges Mid- Ocean Ridges. SEA FLOOR

10. Scientists collected rock samples and determined the shape of the sea floor using a ship named the Glomar Challenger. Ages of rocks youngest rocks were closest to the ridge, oldest rocks were farthest away, next to the continents. Mid Atlantic Ocean Ridge

11. Youngest rocks Oldest rocks

12. C D B A Which rocks are older? A or B C or D

13. Ocean Trenches are DEEP canyons in the sea floor that are parallel to the continent. Ocean Trenches are located close to a plate boundary. Deepest trench on Earth is the Mariana’s Trench next to the Philippine Islands

14. 1.Earth is like a giant Bar Magnetic a)Magnetic north pole is near the geographic north pole b)Magnetic field formed by the motion of the hot molten metal in the outer core 2.Occasionally magnetic poles flip flop: though a process called magnetic reversals. a)Normal polarity: Magnetic north pole points to south Pole b)Reverse polarity: Magnetic south pole point to the north pole c)The cause of reversal s unknown SEA FLOOR MAGNETIC STRIPES

15. Transform Fault Boundary: Occurs where plates scrape past each other. Divergent Boundary: occurs where plates move apart Convergent Boundary: Occurs where plates push together Transformdivergentconvergent

16. Two plates move away from each other leaving a gap between the plates Rift valley Divergent Boundaries A rift valley is a deep valley that forms in the gap between the moving plates Ocean Crust IN THE OCEAN ON LAND

17. New ocean crust is created at Divergent Boundaries as the plates pull away from each other. Krafla Volcano in Iceland Aerial view of the area around Thingvellir, Iceland, showing a fissure zone (in shadow) that is an on-land exposure of the Mid- Atlantic Ridge. Map showing the Mid-Atlantic Ridge splitting Iceland and separating the North American and Eurasian Plates. Divergent Boundaries

18. In the Ocean Mid-ocean Ridges (Also called spreading centers) Rift Valleys Krafla Volcano in Iceland Aerial view of the area around Thingvellir, Iceland, showing a fissure zone (in shadow) that is an on-land exposure of the Mid- Atlantic Ridge. Map showing the Mid-Atlantic Ridge splitting Iceland and separating the North American and Eurasian Plates. Features of Divergent Boundaries

19. On Land Rift Valleys form when continents split If the continents spread far enough apart, new ocean crust will form Features of Divergent Boundaries

20. Mid-ocean ridge Rift valley Newest rock A Older rock B

21. When new crust forms at mid-ocean ridge, the magnetic minerals line up with the earth’s magnetic field. When the magnetic field reverses, the rocks record the new polarity

23. HOT SPOTS are relatively small, long-lasting hot regions where magma rises in plumes. Magma plumes develop into volcanoes that can build up and eventually become a volcanic island or mountain. Hot spots occur far from plate boundaries, yet tell us how fast and in what directions plates are moving. The Hawaiian Islands and Yellowstone are examples of hot spot volcanoes.

25. 1.Ocean crust is destroyed at convergent boundaries at the same rate it is created at Mid-Ocean Ridges. 2.The location where this happens is called the SUBDUCTION ZONE 3.Subduction is when one plate sinks beneath another at a convergent boundary 4.Oceanic crust will subduct under the continental crust 1.Oceanic crust is more dense than continental crust CONVERGENT BOUNDARIES

26. Three types of convergent boundaries –Continental-Continental Convergent –Oceanic-Oceanic Convergent –Oceanic-continental convergent The name tells you the type of crust involved.

27. 1.Continental-Continental Convergence: Creates mountains a)Happens when two continental plates crash together b)Neither plate wants to subduct so the edges crumples forming mountains c)Example: a)India crashed into Asia 50 million years ago b)This caused the Eurasian Plate to crumple up and form the Himalayas c)The collision is still happening. Scientist now know how some types of mountains form.

28. 3. Oceanic-Oceanic Convergence: Creates deep ocean trenches at subduction zones, and island arcs. Deep OceanTrenches occur where two oceanic plates meet; the denser of the two plates will subduct and melt. The magma from the melted palte will rise back to the surface and form an Island Arc Island arc’s are chains of volcanic islands that form on the top plate, parallel to a deep ocean trench. Subduction zone EXAMPLES Mariana trench is the deepest at 36,000 ft below the sea floor. Japan and the Aleutian islands of Alaska are island arc volcanic chain

29. Oceanic-continental convergence: Creates ocean trenches, and coastal mountain ranges Subduction Zone 1.Oceanic -continental subduction occurs where an oceanic plate sinks beneath a less dense continental plate. 2.Deep ocean trenches form where the ocean plate subducts. 3.Coastal mountains from where the less dense continental crust is folded upward. Some of these mountains may form volcanoes. The Cascade mountains, home of Mt. St. Helen, are coastal mountains.

30. 1.The location where plates scrape by each other is called a transform boundary. 2.Crust is neither created nor destroyed, it is just relocated. 3.Most transform faults are found on the ocean floor. 4.They commonly offset the active spreading centers, Transform Boundaries

31. The San Andreas fault is a transform boundary between the North American plate and Pacific plate. The San Andréa's Fault is the reason why California ha sso many Earthquakes Zig-zag pattern on ocean floor

34. Convection is the movement of a material due to rising and sinking of hot and cool materials. Convection Currents create motion of hot molten rock upward and as it cools it sinks down where it is heated again and rises. Convection Currents move the lithosphere only a few centimeters per year, but over a million years plates are carried thousands of kilometers.