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Published byDella Parks Modified over 9 years ago
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Structure of a Continent Figure 13-3
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How are continental plates formed? Figure 13-4
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Why was St. Louis under water during the Cambrian/Ordovician (when the fossils we saw on the field trip formed)? What can cause the ocean level to rise, relative to the land?
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Other continents were as well
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What happens if the plate motions are faster?
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The plates had been moving fast – the ocean seafloor was higher on average, and ocean water spilled up onto continents.
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Continent-Ocean Collision
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Ocean-Ocean Collision
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Antilles Arc
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Subduction Zone Jump
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Granite plutons begin deep within an orogenic belt. How do they get to the surface?
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Granite plutons begin deep within an orogenic belt. How do they get to the surface? Erosion and Isostatic Rebound!
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Tectonic history of North America: Growth of the Appalachians
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Geometry of the Pacific – North America plates
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Western Terranes
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Western Terranes: The Rockies
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But subduction is much more shallow than this picture shows!
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Where does heating come from? Western Terranes: Basin and Range
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Canadian Rockies Appalachians Alps
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Volcanism adds rock to continental volume.
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Hotspot volcanism often begins with a large basaltic flood.
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Columbia flood basalts
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Columbia flood basalts: Beginning of Yellowstone hotspot
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Figure 13.23A
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Figure 13.23B
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Iguazu River Falls (Argentina)
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Shape of Atlantic Ocean determined by Iceland hotspot
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Afar hotspot
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