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Theory of Plate Tectonics Key Vocabulary Lithosphere = Rigid Rock, Crust and upper Mantle Asthenosphere = hot weak zone found within the upper Mantle, allows the Lithosphere to move Rift Valley: found at divergent plate boundaries with continental crust (Red Sea) Seafloor Spreading: occurs at divergent plate boundaries (for example, the Atlantic Ocean is getting larger) Mid Atlantic Ridge Volcanic Island Arcs: at Convergent Plate Boundary, Aleutian Chain, Tonga Islands and Japan Continental Volcanic Arc: at Convergent Plate Boundary, Andes, Cascade Mnts. Driving Mechanisms for Plate Tectonics: Core: upwelling and slab pull Convergent Plate Boundaries : occur when edges of continental or oceanic plates move toward each other and collide. Lithosphere is destroyed. Subduction Zone : when an oceanic plate collides with a continental plate, the oceanic plate bends underneath the continental plate. Convergent Plate Boundaries Continued Deep Sea Trench : forms when the sub ducting plate bends as it sinks. (up to 11 km deep) Divergent Plate Boundaries: occur when plates separate. (midAtlantic ridge) Lithosphere is created. Mid Ocean Ridge : an underwater chain of volcanoes which forms from the less dense rising hot rock moving above the cold and dense oceanic rock. How ocean ridges form Convection Currents Driving Plate Tectonics Two main components 1 Slab Pull: this occurs at Convergent Plate Boundaries. The plate that is more dense gets pulled by gravity downward. This pulls on the rest of the plate behind it. 2 Upwelling: this occurs at Divergent Plate Boundaries. The rising magma hits the surface, forms new rock and pushes the plate around it. Transform Plate Boundaries: occur when plates slide past each other. Lithosphere is neither created nor destroyed. San Andreas Fault Seattle Fault Line on the south end of Bainbridge Island, WA How Do These Plates Move? Convergent Plate Boundary Oceanic Lithosphere (Crust) Divergent Plate Boundary Or Hot Spot Oceanic Trench Oceanic Lithosphere (Crust) Convergent Plate Boundary Oceanic Trench Slab Pull Slab Pull Mantle Plumes Subduction Zone HEAT SOURCE (CORE OF THE EARTH) Subduction Zone Types of Rocks: Igneous - Formed from magma or lava (basalt, granite, obsidian) - crystals Intrusive- Igneous rocks created within the earth Extrusive- Igneous rocks created on the earth's surface Sedimentary - rocks formed by sediments that become compacted (sandstone, limestone) Metamorphic - heat, pressure, time, rocks that are formed below the earth's surface (marble) Seismologist A scientist that studies earthquakes. Earthquake: Vibrations in the earth caused by the sudden release of energy, usually as a result of the movement of rocks along a fault. Seismograph How do scientists locate the epicenter of an earthquake? OPEN NOTE QUICK QUIZ ON PLATE TECTONICS Place a #1 on a clean sheet in your journal and be ready! 1 - Look at the satelite image below and draw a cross section picture of what is occuring. Make sure you label the following: type of plate boundary, the oceanic trench, subduction zone and volcanoes. 2 - What is the name for a chain of volcanoes that are on continental crust? 3 - What is the name for a chain of volcanoes that come out of oceanic crust that have the same plate boundary as question #2. 4 - What common type of plate boundary is found near the above volcanic chains? 5 - What are the two categories of igneous rocks? 6 - The islands of Hawaii were formed by magma rising to the earth's surface. This point on the surface is a called a ______________. A B C D E 7 - Which island above has the oldest rock? A,B,C,D, or E? Label the following with the type of plate boundary that the red arrow is pointing to. 8 - ___________ 9 - ______________________ Green Arrows show the direction the plates are moving. 10 - _________________ Extra Credit What type of volcanoes are these... 1 ____________ 2 ____________ 3 ________________