Drifting of Continents and Plate Tectonics
ICSE · Class 11 · Geography
Complete topic list for Drifting of Continents and Plate Tectonics in ICSE Class 11 Geography. Key concepts, sub-topics, and what to focus on for board exams.
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Topics in Drifting of Continents and Plate Tectonics
Wegener's Continental Drift Theory
- Alfred Wegener (1912, revised 1924) proposed that continents were once joined together in a supercontinent called Pangaea (meaning 'all lands')
- Pangaea existed in the Upper Carboniferous period, approximately 250-300 million years ago
- The supercontinent was surrounded by a vast ocean called Panthalasa
Evidence Supporting Continental Drift Theory
- Mountain belts: Ancient mountain systems (470-350 million years old) now separated by Atlantic Ocean show continuity when continents are reassembled
- Fossil evidence: Similar fossils found on continents now separated by vast oceans - Glossopteris (plant), Mesosaurus and Lystrosaurus (animals) found in India, Australia, South Africa, South America,
- Geological matching: Gold deposits in Ghana (Africa) match with gold-bearing veins in Belen Sau (Brazil) across 5,000 km of Atlantic Ocean; no source rocks in Ghana indicate gold was transported from
Criticisms and Limitations of Continental Drift Theory
- Jig-saw-fit is imperfect: Gap of about 15° exists between South America and Africa when positioned together
- Direction of drift unclear: Wegener proposed westward and equatorward drift, but other scientists (F.B. Taylor, J.W. Evans) proposed different directions of drift
- Inadequate forces: Two forces suggested by Wegener (tidal force and differential gravitational force) are mathematically insufficient; tidal force would need to be 10,000 million times more powerful,
Sea Floor Spreading
- Disintegration of Pangaea occurred over the last 65 million years
- Continental drift process continues today at measurable rates
- Mid-oceanic ridges are cracks on ocean floors where molten rocks (magma) push upward from the mantle
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