Download presentation
Presentation is loading. Please wait.
Published byTeresa Andrews Modified over 9 years ago
1
Plate Tectonics (Wrong kind of plate…and where’s my salad fork?)
2
The crust is broken!
4
We measure plate motion with GPS
5
Continental Drift Whiplash
6
Plate Boundary Types
7
Divergent plate boundary
8
2 plates are moving AWAY from each other2 plates are moving AWAY from each other Seen in mid-ocean ridgesSeen in mid-ocean ridges and rift valleys and rift valleys Where in the world?
9
Divergent plate boundary (forming a rift valley)
10
Mid ocean ridge
11
Divergent plate boundary Features: 1) 1) 2) 2) 3) 3)
12
Divergent plate boundary Features: 1)Mid ocean ridges 2)Undersea volcanoes—may make islands 3)Rift valleys, on land
13
Convergent plate boundaries
14
2 plates move TOWARD each other2 plates move TOWARD each other
15
What is happening at the plate boundary? Oceanic Plate
16
Subduction When 2 plates converge, one plate MAY move downwards UNDER the other – this is called SUBDUCTIONWhen 2 plates converge, one plate MAY move downwards UNDER the other – this is called SUBDUCTION
17
Subduction Earthquakes are deeper the farther inland you go.
18
Subduction Accretion—some of the lightest oceanic crust joins the continent
19
Which plate is subducting?Which plate is subducting? What is happening to the subducted plate?What is happening to the subducted plate?
20
Convergent plate boundaries Features: 1) 1) 2) 2) 3) 3)
21
Convergent plate boundaries
23
Features: 1) …in ocean/ocean convergences 2) …in ocean/continent convergences 3) …in continent/continent convergences
24
Convergent plate boundaries Features: 1)Ocean trenches and volcanic island arcs 2)Benioff zone earthquakes, continental rim volcanoes and accretion 3)High plateaus, thrust faults and mountains
25
Transform plate boundary 2 plates slide past each other2 plates slide past each other Pacific Plate North American Plate
26
Transform Plate Boundaries The area where these plates meet is called a transform faultThe area where these plates meet is called a transform fault The San Andreas Fault in California is possibly the most famousThe San Andreas Fault in California is possibly the most famous
27
Transform Plates
30
Point Reyes, California
31
Transform plate boundaries Features: 1) 1) 2) 2) 3) 3)
32
Transform plate boundaries Features: 1) Major earthquakes 2) Offset linear features 3)Fracture zones
33
What kind of boundary? 12345
34
What features do they make? 12345
35
Plate Boundary Types
36
Why do the plates move? 1) 2) 3)
37
Why do the plates move? 1)Heat 2)Differences in density 3)Gravity
38
Why do the plates move? Inner core Outer core Mantle Crust Mantle and outer core are melted
39
Heat The Earth was originally molten The heat within the Earth is left over from then Radioactivity adds some heat
40
Density D=mass/volume Less dense floats on more dense If you heat an object or fluid, it expands, the density decreases A more dense fluid will force a less dense to rise
41
The average density of the Earth provides evidence of the relative densities of the different layers of Earth - crust, (lithosphere) -mantle (asthenosphere) and -core.
42
The average density of the Earth provides evidence of the relative densities of the different layers of Earth - crust, (lithosphere) -mantle (asthenosphere) and -core. The whole Earth is more dense than the rocks we see
43
Density Mantle is more dense than crust Oceanic crust is more dense than continental crust
44
Gravity g=Gm 1 m 2 /d 2 If anybody cares. What we do care about is that a) if you heat a fluid, its density decreases, b) the cooler fluid is more dense, so it sinks.
45
All together-- Convection happens!
46
Why do the plates move?
47
Convection happens!
48
The accepted mechanism for plate motion is: convection in the asthenosphere. Convection happens!
49
This plate is pulled this way…
50
Convection happens! …and this plate is pulled this way.
51
Wegener’s Evidence Wegener supported his hypothesis of continental drift with evidence from the puzzle fit of the continents, rock units, geologic structures, fossils and glacial evidence.
52
Evidence The modern theory of plate tectonics is supported by evidence from:
53
Evidence The modern theory of plate tectonics is supported by evidence from: A.paleomagnetism, B. C. D. a. b. c. Seafloor crust shows the direction of the magnetic field when the crust was formed
54
Evidence The modern theory of plate tectonics is supported by evidence from: A.paleomagnetism, B.age of ocean floor sediments C. D. a. b. c. Seafloor crust is older farther from the mid-ocean ridge
55
Evidence The modern theory of plate tectonics is supported by evidence from: A.paleomagnetism, B.age of ocean floor sediments C.ocean floor topography D. a. b. c. You can see the ridge and the suture zone around it
56
Evidence The modern theory of plate tectonics is supported by evidence from: A.paleomagnetism, B.age of ocean floor sediments C.ocean floor topography D. Wegener's evidence. a. b. c. Wegener had none of the above. He had to do it the hard way
57
Evidence The modern theory of plate tectonics is supported by evidence from: A.paleomagnetism, B.age of ocean floor sediments C.ocean floor topography D. Wegener's evidence. a.fossils b. c. Tropical fossils show up in polar regions
58
Evidence The modern theory of plate tectonics is supported by evidence from: A.paleomagnetism, B.age of ocean floor sediments C.ocean floor topography D. Wegener's evidence. a.fossils, b.jigsaw continents, c. They fit together pretty well
59
Evidence The modern theory of plate tectonics is supported by evidence from: A.paleomagnetism, B.age of ocean floor sediments C.ocean floor topography D. Wegener's evidence. a.fossils, b.jigsaw continents, c.rock types Similar rocks show up on different continents
Similar presentations
© 2025 SlidePlayer.com. Inc.
All rights reserved.