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THEORY OF CONTINENTAL DRIFT |
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1912. The continents were once joined and slowly drifted apart. Not accepted until 1960. |
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1880-1930. Meterologist. Coined continental drift and sea-floor spreading |
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EVIDENCE FOR CONTINENTAL DRIFT |
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1. Matching coastlines-fits like puzzle. 2. Fossil evidence-glossopteris/fern leaf. 3. Evidence from rocks 4. Climatic evidence-equator has glacial scars. |
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1920. Lithosphere divided into 7 major plates. Plates float on aesthenosphere. Plates move in different directions depending on weight and size. Links continental drift and sea-floor spreading. |
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Magma and energy rotating. Makes more heat. Proves continental plates move and that new floor is "made." |
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1950. Harry Hess. Ocean floor moves away from ridge, magma rises, cools and replaces with "new" ocean floor. Robert Diaz coined the term. |
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ROBERT DIAZ AND HARRY HESS |
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Sea-floor spreading. Hess "discovered it. Diaz coined term. |
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MAGNETIC BANDS ON OCEAN FLOOR |
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The variation in iron being up welled. Switches polarity(not literally). It can help tell the age of a rock. |
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Underwater mountain range in the Atlantic Ocean. |
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"Comes together"-Compression. |
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A fracture along which visible displacement can be detected on one side relative to the other. |
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A series of ripples that result from compressional deformation of the lithosphere. |
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Stress-Tension. Boundary-Divergant. Great Rift Valley, Africa. |
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Stress-Compression. Boundary-Convergant. Andes Mts. |
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Stress-Shearing. Boundary-Transform. *San Andres Fault. |
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GREAT RIFT VALLEY, AFRICA |
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The vibrations of the Earth's surface that carry energy. |
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Above the focus(surface), most violent area of shaking. Usually around the origin of the earthquake. |
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Place along fault where crust "slips"; Also the origin of the seismic waves. |
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Carry energy and create the damage in and Earthquake. 1. P-waves 2. S-waves 3. L-waves |
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*Primary Waves(slinky). *Push-Pull(compression)waves *Fastest *First to arrive *Travels through solid, liquid, gas. *Weakest. |
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*Secondary Waves(Snake). *Side to side(transverse)waves. *Second fastest(slower than Pwaves). *Second to arrive. *Travels through solids only. *Stronger than Pwaves. |
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*Love Waves(Surface Waves). *Up and Down motion. *Slowest. *Travels along Earth's surface. *Strongest. *Most destructive. |
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Measurement of the magnitude in an earthquake. |
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The difference in time(arrival). |
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A major fault line in California. |
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A mountain that forms when layers of lava and volcanic ash build up and erupt. |
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Crust under the Ocean. Denser than Continental crust. |
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Crust under continents/"Land Continents". Less dense than oceanic crust. |
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*Layers. *Filled central vent. *Radiating dikes. |
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*Steep sided *Piles of tephra -Tephra- the hardened lave that was thrown from the volcano. *Large indention. *Breaks off into different sections in a large area. |
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*Quiet eeruptions *Broad volcano with gently sloping sides. *Hawaiian Islands and Iceland. |
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*Causes explosive eruptions. *Tends to harden in vents. *Causes pressure build-ups. |
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*Thin and runny. *Thick and viscous; slower, slimey |
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