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Physical Science Question: How can magnetism of rocks provide evidence of continents moving?

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Presentation on theme: "Physical Science Question: How can magnetism of rocks provide evidence of continents moving?"— Presentation transcript:

1 Physical Science Question: How can magnetism of rocks provide evidence of continents moving?

2 Wednesday Connecting the rube to the physics assignment And Answers to 10 class questions Rube Check continental drift evidence Plate Tectonics

3 Homework assignment Use the internet and book to find descriptions of the following concepts: PangaeaDivergent boundary PanthalassaConvergent Boundary Continental driftRift Valley MesosaurusSubduction Zone Mid-Atlantic RidgeOcean Trench MagmaTransform Boundary Sea-floor spreading Paleomagnetism

4 What evidence is there that the continents have moved in the past? In other words, what evidence is used to support the continental drift theory

5 Evidence 1) 2) 3) 4) 5)

6 Evidence 1)Physical shape of continents 2)Rock evidence of change in climate 3)Fossil evidence, including Mesosaurus 4)Difference in ages of oceanic crust vs continental crust 5)Paleomagnetism of rock on either side of the Mid Atlantic ridge

7 Alfred Wegener

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10 Determining the magnetic orientation of ocean rock

11 In the 1950’s and 1960’s…. Used Sonar (invented during WWII) to map the Ocean Floor To Produce underwater maps for Submarines Found that there was a huge ridge of mountains in the middle of the Atlantic ocean

12 Have found many examples since Of these mid Oceanic ridges around the world Volcanically active (but not wholly destructive) Ocean floor is not smooth as once thought

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14 Paleomagnetism Study of the Earth’s magnetic record over time Minerals in hot rocks do not have a set magnetic direction As it cools, the magnetic orientation of those minerals becomes fixed pointing in the direction of the “North Pole”

15 This magnetic orientation can and has be measured

16 What is magnetic orientation? Means the direction that the rock makes a compass point as it passes over

17 What has been discovered… Discovered bands of rock with different magnetic orientation as the ship moves away from ridge Evidence that the orientation reverses every 200,000 to several million years Matched bands with the same magnetic orientation are found on both sides of a ridge

18 Orientation of rocks around a ridge

19 Different colors represent rocks of different geologic age

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21 Iceland on a diverging plate boundary

22 Who wants to act?

23 What is the best explanation for the matched bands of rock? New ocean floor is being produced from the ridge Older material material is pushed away from ridge by newer material This in turn moves the continents apart

24 Mid ocean Ridges Are the place of creation of new plate material Boundary between plates As plates are created items on the plates are moved farther away from the ridge Divergent boundary

25 Sea-floor Spreading Driven by the introduction of new material at the ridges, the older sea floor is pushed away from the ridges. The oldest ocean rock is farthest away from the ridges The coldest and most dense rock is farthest away from the ridges

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27 If new crust material is being created… Old material must be destroyed because the surface area of the earth is not increasing

28 Where do plates come together? Convergent boundary Subduction zones Most have a lot of volcanic and earthquake activity associated with their interaction

29 What happens at a subduction zone? The density of material coming together determines what happens The most dense material is pushed under the least dense material

30 Variations in Convergent boundaries Ocean to continental crust Continental to continental Ocean to Ocean crust

31 Oceanic meets Continental crust The west Coast of the US around Seattle and Portland

32 West Coast

33 Ocean-vs-Continent More dense ocean crust is push beneath Continental crust When it is pushed deep enough it begins to melt The melted material is pushed upward, supplies material for volcanos

34 Magma and Lava Magma Lava

35 Continental material meets other continental material The mountains between India and China

36 Subduction zone –The Himalayas

37 Continent –vs-Continent Nothing is pushed down much, similar density Build Mountains Keep building as long as pushing occurs No volcanos

38 Ocean-vs-Ocean All based on age of rock, the oldest material is pushed under Creates volcanic islands, or island ars

39 Subduction zone - Japan

40 One final type of boundary interaction TRANSFORM BOUNDARY

41 Southern California San Andreas Fault

42 Transform Moves past each other Not creating or destroying material Earthquakes

43 Plate Tectonics Describes continental movement Describes why and how continents move

44 Plates and Continents

45 Pangaea and Panthalassa


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