the theory of continental drift. homework: complete puzzle and “position” paper (1 full pg). due...
TRANSCRIPT
Continental Drift TheoryContinental Drift Theory
• Proposed by Alfred Wegener in 1912
• 250 million years ago, all of the continents were combined into one super-continent called “Pangaea”
• The continents gradually drifted apart to where they are today
Evidence of Continental DriftEvidence of Continental Drift
Puzzle Pieces• Continents look like
they could be part of a giant jigsaw puzzle
• Continental shelves
of Africa and South America fit together almost perfectly
Distribution of FossilsDistribution of Fossils• The Fossil Record
– Glossopteris remains found in SA, Australia, Asia, and Africa, & Antarctica
– Fossils of deciduous trees found near North Pole
– Coal formation in many parts of the world, but needed to be swampy marshes with lots of rain near the equator
Sequence of Rock TypesSequence of Rock Types• The Rock Record• Rocks in Argentina
identical to ones in Africa• Diamond rich rocks in
South Africa match rocks in Brazil
• Coal beds in NA, Britain, and Belgium same
• Red sandstone same in NA, Greenland, Britain, Norway
Ancient ClimatesAncient Climates
• Tropical plant remains (coal deposits) found in Antarctica
• Glaciation in Africa, South America, India, and Australia during the same time
Theory of Continental DriftTheory of Continental Drift
• Vocabulary– Continental shelf – part of a continent that
extends under shallow water from the ocean’s edge to the steeper sea floor slope.
– Pangaea- all land– Panthalassa – all seas– Theory of Continental Drift – continents were
once one landmass that broke apart and moved to present locations.
Evidence of Continental DriftEvidence of Continental Drift
• 1. Puzzle Pieces – continents fit together like a giant puzzle – esp. SA and Africa
• 2. Fossil Record – the same plants, trees, and animals and coal beds occur in different continents
• 3. Rock Record – same sequence of rock occurs on different continents, same mountain ranges occur on different continents
• 4. Climate – same glaciation marks on different continents, fossil indicate tropical climates where now cold.