Continental Drift, Lecture notes of Earth Sciences

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 Drift
Theory of Continental DriftTheory of Continental Drift
Theory of Continental Drift
Continental Drift
Continental DriftContinental Drift
Continental Drift
Alfred Wegener
1912
Theory that all landmasses were once joined: Pangaea
Evidence of Continental Drift
Evidence of Continental DriftEvidence of Continental Drift
Evidence 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
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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