Continental Drift Notes (Chapter 7 Section 1)

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Continental Drift Notes (Chapter 7 Section 1) I. Important Terms: Pangaea: means All Land Continental Drift: All continents were once connected in a single large landmass. They broke apart about 200 million years ago and drifted apart to their current positions. II. Alfred Wegener – Developed Theory of Continental Drift • Alfred Wegener was a German meteorologist (studied weather) credited with development of the Continental drift theory. • Wegener observed the east coast of South America and the west coast of Africa fit together like puzzle pieces. • His ideas were NOT accepted by other scientists of his time. o The missing piece from his theory was sea floor spreading (the How?). Wegener did not have the technology to travel to the sea floor and collect samples of rock. o It was not until after his death that evidence was gathered to support his theory and his theory was finally accepted. III. Wegener’s Evidence to Support his Theory of Continental Drift • The puzzle-like fit of the South America and Africa • Fossils and Plants o Fossils of Mesosaurus (a fresh-water, land-dwelling reptile) were found in both Africa and South America. § How can it get across a great body of salt water? o Fossils of Glossopteris (a tropical, fern-like plant) were found in Antarctica, Australia, India, South America and Africa. § Strange? Tropical meaning warm temperatures and high humidity; Antarctica meaning cold temperatures and no sunlight for part of the year § Is this possible? o Other fossil evidence exists as well. (Fossil Safari) More Evidence that Supported Wegener’s Theory of Continental Drift… • Climate Clues o He found evidence of glaciers in tropical areas. o Glacial deposits and scoured (scratched) rock surfaces were found in S. America, Africa, India and Australia. § How can you explain the presence of glacial deposits in areas were no glaciers exist today? • Rock Clues o Similar rock structures are found on different continents. § Examples: • The same age and type of rocks from the Appalachian Mountains are also found in Greenland and Western Europe. • Similar rocks are found along the coast of South America and Africa. Fossil Evidence Rock Evidence .

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