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Plate Tectonics. Chapter 3, part 2. Last Time. Expanding Earth Contracting Earth Continental drift hypothesis Sea floor spreading. What drives plate movement?. Late 1900’s : Plate tectonics Crust: cold, rigid Mantle: hotter, behaves plastically. What drives plate movement?.
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Plate Tectonics Chapter 3, part 2
Last Time • Expanding Earth • Contracting Earth • Continental drift hypothesis • Sea floor spreading
What drives plate movement? • Late 1900’s: Plate tectonics • Crust: cold, rigid • Mantle: hotter, behaves plastically
What drives plate movement? • Ultimately: heat transported from core and mantle to surface • Heat transported by convection • Core is ~5,000°C and surface is ~0°C • Mantle convection creates a conveyor belt in mantle • Crust dragged along on top
Plate movement with convection • Where mantle rises: rifting • Where mantle dives: subduction zones
Theory of plate tectonics • Crust made of rigid plates • Ocean plates: thin and dense • Continental: thicker, less dense • Plates are moving on top of mantle
Theory of plate tectonics • Crust made of rigid plates • Ocean plates: thin and dense • Continental: thicker, less dense • Plates are moving on top of mantle • Plates separate and collide
Types of plate boundaries • Divergent: plates move apart • Convergent: plates collide • Transform: plates slide by each other
Divergent Plate boundaries • A.k.a. spreading ridges
Evidence of divergent plate boundary in oceans • Pillow lavas of basalt along mid-Atlantic ridge
Convergent plate margins • 2 plates meet head on
Ocean-ocean convergence • One plate dives down (subducts) below other plate • Volcanoes form above subduction zone • Basalts • Volcanic island arc
Ocean-ocean convergence • One plate dives down (subducts) below other plate • Volcanoes form above subduction zone • Basalts • Volcanic island arc • Aleutians, Japan etc.
Convergent plate boundaries • Ocean-continent convergence • Ocean plate subducts below continent
Ocean-continent convergent margin • Melting forms volcanoes above subduction zone • Forms rhyolites, andesites
Ocean-continent convergent margin • Melting forms volcanoes above subduction zone • Forms rhyolites, andesites • Cascades, Andes
Continent-continent convergence • Neither plate wants to subduct • Lots of metamorphic rocks, lots of folds, high mountains
Continent-continent convergence • Neither plate wants to subduct • Lots of metamorphic rocks, lots of folds, high mountains • Himalaya, Alps
How to recognize ancient subduction zone? • Volcanic rocks, andesites • Deformed ocean sedimentary rocks
Transform plate margin • 2 plates slide past each other
Transform boundary and earthquakes • The division between two blocks is called a fault • Strain builds up in rocks due to friction • Rocks rupture releasing strain in the form of earthquake energy
Transform boundary and earthquakes • The division between two blocks is called a fault • Strain builds up in rocks due to friction • Rocks rupture releasing strain in the form of earthquake energy
How to recognize ancient transform boundaries • Broken, ruptured rock • Adjacent rock units that shouldn’t be next to each other
How are plate movements determined? • Satellite/GPS • Age of ocean floor, distance from spreading ridge • Distance= rate x time
Plate tectonics • Controls where mountains are built • Controls where earthquakes are • Controls biologic world (climate, geographic barriers)
Plate tectonics homework 3 PM Friday • Scavenger hunt by 3 PM Wednesday • Potential test question today • Name • Question from tectonics or rocks lectures you want to see on the first test.
Where are earthquakes? • Transform boundaries • Subduction zones • Areas of active mountain building
Where are areas of active mountain building? • Collision zones between plates • Volcanoes, earthquakes, deformed rocks