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Continental Drift. Continental Drift. Alfred Wegener. 1912. Theory that all landmasses were once joined: Pangaea. Evidence of Continental Drift.
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Theory of Continental DriftTheory of Continental DriftTheory of Continental DriftTheory of Continental Drift
Continental DriftContinental DriftContinental DriftContinental Drift Alfred Wegener 1912 Theory that all landmasses were once joined: Pangaea Evidence of Continental DriftEvidence of Continental DriftEvidence of Continental DriftEvidence of Continental Drift
Coastlines Coasts of Africa and South America (among others) match like puzzle pieces
Mountain Chains Ancient mountain chains match up across continents
Coal Fields Fields in Brazil match those in Africa
Glacial Deposits Deposits of material from glaciers match in Africa, India, South America, Australia and Antarctica
Glacial Deposits Found in tropical climates Glacial Striations Grooves carved by glaciers match up in various continents
Climate changes Deposits not fitting climate Salt- too far from equator Coral- non-tropical areas Coal in cold, dry areas
Fossil Evidence Fossils of organisms out of climates survive in Glossopteris Plant- seed dispersal;arctic area Lystrosaurus Reptile in arctic regions
Weakness of TheoryWeakness of TheoryWeakness of TheoryWeakness of Theory Wegener could not explain how continents moves
Acceptance of Theory Occurred when understood Earth’s structure Core Mantle Asthenosphere Crust/Lithosphere Earth’s tectonic plates Movement of PlatesMovement of PlatesMovement of PlatesMovement of Plates Interior of Earth hot-radioactivity Creates convection currents Crust “floats” on asthenosphere of mantle Convection Currents Movement of Plates
Isostacy Balance between upward force of mantle and downward force of crust Earth’s Crust and Isostacy Oceanic crust more dense Float lower on mantle Continental crust less dense Float higher on mantle