1. Plate Boundaries

2. Review: Wegener's proposal Wegener - continental drift hypothesis 4 lines of evidence Continental puzzle Fossil records Matching mountain ranges Ancient climate Main objection to Inability to provide a logical mechanism

3. Earth’s internal structure Earth’s internal layers can be defined by Chemical composition Physical properties Crust two types  Continental  Oceanic (denser) Mantle  82% of the volume of the Earth Core solid Iron & nickel

4. Density Density is a physical property that ties most things on earth together? Anything that works through convection currents Plate movements ocean currents Weather

5. Earth’s internal structure Four main layers of Earth based on its physical properties and mechanical strength are: Lithosphere Asthenosphere Mesosphere Core

6. Earth’s internal structure  Lithosphere Solid crust and small part of the mantle stuck to the crust  Asthenosphere Hotter and more fluid than lithosphere Allows for motion of lithosphere above

7. Plate Boundaries  3 Types of plate boundaries Divergent plate boundaries (constructive margins) Convergent plate boundaries (destructive margins) Transform fault plate boundaries

8. Plate boundaries  Divergent plate boundaries (constructive margins) Two plates move apart as a result of the mantle material upwelling from convection. Key Features: Oceanic Ridges - develop along well- developed boundaries or ridges, the seafloor spreads apart and creates new crust. Rift Valleys – found on land where continent is being ripped apart. Examples Iceland The East African rift

9. Divergent boundaries Figure 15.10 They are located most on mid-oceanic ridges

10. Rift Valleys

11. Oceanic-continental convergent plate boundary Denser oceanic slab sinks into the asthenosphere Pockets of magma develop and rise as a result of carbon and water pulled down with the subducting plate.. Key Features: Continental Volcanic Arcs or (Volcanic mountain ranges) Examples: Andes & Cascades Ocean Trench: form as lithosphere is subducted into the mantle.

12. Oceanic-oceanic convergent plate boundary Two oceanic slabs converge and one descends beneath Key Features: Volcanic Island Arcs: form as volcanoes emerge from the sea floor from subduction. Example: Japan and Alaskan Island Chain (NOT Hawaii!) Deep Ocean trenches Example: marians trench

14. Continental-continental convergent plate boundary Figure 15.14 C Two continents collide both made of lower density rocks and neither wants to subduct as a result the material lifts up into very high mountain ranges. Key Feature: Very tall non-volcanic mountain ranges Example: Himalayas

15. The collision of India and Asia produced the Himalayas Figure 15.15 A Before After

16. Transform fault boundaries  Plates slide past each other, no new crust is created or destroyed.  Most are found perpendicular to mid-ocean ridges as they Aid in the movement of divergent boundaries. Most Famous Example: San Andreas Fault