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The Earth’s Interior
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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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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)
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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
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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
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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
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Earthquake 1/6/14
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IV. Measuring Earthquakes A. Seismograph 1.Device which measures seismic waves Clicker ?’s 1-9
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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
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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
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Divergent Boundaries
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Divergent Boundaries- can observe reverse polarity
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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
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Convergent Boundaries
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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)
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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)
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VI.Earth’s internal layers A. Geologists did research with seismic waves B. Concluded that the Earth’s interior is layered.
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Earth’s internal layers SKETCH THIS!
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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
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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.
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B. The Mantle A. Rocky layer B. About 3000 km thick
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Mantle (cont.) a. Lower mantle b. Upper mantle – two sections two sections
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Upper mantle (cont.) 1. Asthenosphere - behaves in a semi-fluid manner
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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
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Thickness of layers.
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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
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The Crust (cont.) b. Continental crust – below land, less dense about 20-60 km thick
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Evidence that supports the theory of Continental Drift 1. Geologic (rock) 2. Biologic (life) 3. Climatological (past weather) 4. Continental Shelves fit together well
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Tectonic Plates moving sections of the lithosphere on which continents lie on which continents lie
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Major Tectonic Plates Clicker ?’s 1-9 (Continental Drift and Faults)
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