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The Earth’s Interior. Write down the things that are in yellow Other terms in this PowerPoint are helpful but do not need to be included in your notes.

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Presentation on theme: "The Earth’s Interior. Write down the things that are in yellow Other terms in this PowerPoint are helpful but do not need to be included in your notes."— Presentation transcript:

1 The Earth’s Interior

2 Write down the things that are in yellow Other terms in this PowerPoint are helpful but do not need to be included in your notes.

3 I.Plate tectonics- describes movement of the crust (theory) A. Continental Drift- the continents have drifted from one location to another B. Continents used to be in one mass called Pangea (250 mill. Years ago)

4 II.Earthquakes A. Seismic Waves – generated waves traveling through the Earth’s interior B. These waves give us clues to the composition of the Earth

5

6 III. III. Types of waves A. P-waves (primary waves) 1.Compress and expand rock 2.Are the fastest 3.First waves to register on seismograph

7 Types of waves (cont.) B. S-waves (secondary waves) 1. Vibrate up and down or side to side 2.2 nd waves to register on a seismograph S Waves

8 Earthquake 1/6/14

9 IV. Measuring Earthquakes A. Seismograph 1.Device which measures seismic waves Clicker ?’s 1-9

10 V.Movement along a fault boundary  Transform-fault boundary – plates are sliding past one another plates are sliding past one another EX. San Andreas fault in California fault in California ★ Earthquakes caused by shearing forces

11 V.Movement (cont.) B. Divergent Boundary 1. two plates are moving apart 1. two plates are moving apart  Plate A Plate B   Plate A Plate B  2. Forms rift valleys - large spreading valleys 2. Forms rift valleys - large spreading valleysor 3. Creates sea floor spreading- a rift valley on sea floor 3. Creates sea floor spreading- a rift valley on sea floor 4. Caused by tensional forces 4. Caused by tensional forces

12 Divergent Boundaries

13 Divergent Boundaries- can observe reverse polarity

14 V.Movement (cont.) C. Convergent Boundaries 1. 2 plates move towards each other Plate A   Plate B Plate A   Plate B 2.Leads to subduction- one plate (usually oceanic crust) (usually oceanic crust) goes beneath the other goes beneath the other (continental crust). (continental crust). a.Caused by compressional forces

15 Convergent Boundaries

16 Ex: Andes Mountains in S. America (Still growing because of subduction) (Still growing because of subduction) 3. ★ Common place to find volcanoes Ex: Cascade Range (Mt. St. Helens & Mt. Rainier)

17 Quiz Time!- word bank (some > 1) Transform Boundary Convergent Boundary Divergent Boundary Continental Crust 2. 5. 4. 3. 6. Crust type 7. Crust type 1. 8. Oceanic Crust Subduction Rift Valley (divergent)

18 VI.Earth’s internal layers A. Geologists did research with seismic waves B. Concluded that the Earth’s interior is layered.

19 Earth’s internal layers SKETCH THIS!

20 Earth’s internal layers A. Core- 1. Composed mostly of iron and nickel 1. Composed mostly of iron and nickel 2. Inner Core 2. Inner Core very hot very hot solid Fe & Ni due to high pressure of the Earth solid Fe & Ni due to high pressure of the Earth

21 The Core (continued) 3. Outer Core 3. Outer Core  less pressure from the earth  liquid Fe & Ni  Flow in the outer core generates an electric current that powers the Earth’s magnetic field.

22 B. The Mantle A. Rocky layer B. About 3000 km thick

23 Mantle (cont.) a. Lower mantle b. Upper mantle – two sections two sections

24 Upper mantle (cont.) 1. Asthenosphere - behaves in a semi-fluid manner

25 Upper mantle (cont.) Lithosphere- rigid and brittle Source: http://www.uwsp.edu/geo/faculty/ritter/images/lithosphere/tectonics/earth_structure.jpghttp://www.uwsp.edu/geo/faculty/ritter/images/lithosphere/tectonics/earth_structure.jpg Legend Lithosphere & Crust Mantle & & & Asthenosphere Outer Core Inner Core

26 Thickness of layers.

27 C. The Crust  Uppermost portion of the lithosphere  Two types of crust a. Oceanic crust – below ocean, dense a. Oceanic crust – below ocean, dense about 10 km thick

28 The Crust (cont.) b. Continental crust – below land, less dense about 20-60 km thick

29 Evidence that supports the theory of Continental Drift 1. Geologic (rock) 2. Biologic (life) 3. Climatological (past weather) 4. Continental Shelves fit together well

30 Tectonic Plates moving sections of the lithosphere on which continents lie on which continents lie

31 Major Tectonic Plates Clicker ?’s 1-9 (Continental Drift and Faults)


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