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HISTORY OF THE CONTINENTS
Grotzinger • Jordan Understanding Earth Seventh Edition Chapter 10: HISTORY OF THE CONTINENTS © 2014 by W. H. Freeman and Company
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History of the Continents
Chapter 10: History of the Continents
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About Evolution of the Continents
Nearly two-thirds of the Earth’s surface – all of the oceanic crust – was formed over the past 200 million years. However, rocks of the continents are much older, as old as 4 billion years. Studying the continents tells us how the continental lithosphere formed and evolved.
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Lecture Outline The structure of North America
2. Tectonic provinces around the world 3. How continents grow 4. How continents are modified 5. Origin of cratons 6. Deep structure of the continents
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● The stable interior ● Canadian shield ● interior platform
The Structure of North America ● The stable interior ● Canadian shield ● interior platform ● basins and uplifts
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The Structure of North America
● The Appalachian fold belt ● Valley and ridge province ● Blue ridge province ● Piedmont ● Coastal Plain & Continental Shelf
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● The North American cordillera ● uplift and orogeny ● rejuvenation
The Structure of North America ● The North American cordillera ● uplift and orogeny ● rejuvenation ● crustal stretching
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● Continental geology ● cratons ● orogens ● passive margins
2. Tectonic Provinces around the World ● Continental geology ● cratons ● orogens ● passive margins ● active margins
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● Types of tectonic provinces ● shield ● platform ● continental basin
around the World ● Types of tectonic provinces ● shield ● platform ● continental basin ● orogen ● extended crust
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● Ages of tectonic provinces ● Archean ● Early Proterozoic
around the World ● Ages of tectonic provinces ● Archean ● Early Proterozoic ● Middle Proterozoic ● Late Proterozoic ● Paleozoic ● Mesozoic and Cenozoic
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Thought questions for this chapter
Figure 10.8b shows more continental crust of Mesozoic-Cenozoic tectonic age than continental crust of any geologic period. Does this contradict the hypothesis that most of the continental crust was differentiated from the mantle in the first half of Earth’s history?
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● Continental accretion ● accreted terrains ● exotic terrains
3. How Continents Grow ● Modes of growth ● Magmatic addition ● Continental accretion ● accreted terrains ● exotic terrains
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Terrain accretion
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Terrain accretion Spreading center (divergent boundary)
Aleutian Trench Wrangellia Spreading center (divergent boundary) Subduction margin (convergent boundary) Cascadia Trench Transform fault N O R T H A M E R I C A San Andreas Fault Island arc Submarine deposits Ancient ocean floor Displaced continental fragments
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Thought questions for this chapter
How would you recognize an accreted terrain? How could you tell if it originated far away or nearby?
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● Modification by plate collision ● Alpine-Himalayan orogeny
4. How Continents Are Modified ● Modification by plate collision ● Alpine-Himalayan orogeny ● Assembly of Pangaea ● The Wilson Cycle
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Alpine-Himalayan Orogeny
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Alpine-Himalayan Orogeny
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Alpine-Himalayan Orogeny
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Alpine-Himalayan Orogeny
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Alpine-Himalayan Orogeny
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Wilson Cycle
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Geologic Time Scale of Events in the History of Earth’s Continents
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● Modification by epeirogeny ● cooling and heating of lithosphere
4. How Continents Are Modified ● Modification by epeirogeny ● cooling and heating of lithosphere ● weight of accumulating sediments or glacial ice
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Thought questions for this chapter
How would you identify a region where active orogeny is taking place today? Give an example. Would you prefer to live on a planet with orogenies or without them? Why?
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● granite-greenstone terrains
5. Origin of Cratons ● Archean cratons ● granite-greenstone terrains ● high-grade metamorphic terrains
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Thought questions for this chapter
Why are the ocean basins just about the right size to contain all the water on Earth’s surface?
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● Structure of the craton ● continental crust ● cratonic keel
6. Deep Structure of the Continents ● Structure of the craton ● continental crust ● cratonic keel
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Thought questions for this chapter
What would happen at the surface if the cold keel beneath a craton suddenly heated up? How might this effect be related to the formation of the Colorado Plateau?
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Key terms and concepts Accretion Active margin Craton Cratonic keel
Accreted terrain Accretion Active margin Craton Cratonic keel Epeirogeny Glacial rebound Magmatic addition Orogen Orogeny Passive margin Rejuvenation Shield Tectonic age
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Key terms and concepts Tectonic province Wilson cycle
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