1. Warm-up What are the phases of the moon starting with the New Moon? Draw them.

3. Vocabulary Words Asthenosphere-plasticlike layer of Earth on which the lithospheric plates float and move around Continental drift- Wegener’s hypothesis that all continents were once connected in a single large landmass that broke apart about 200 million years ago and drifted slowly to their current positions Convection current- current in Earth’s Mantle that transfers heat in Earth’s interior and is the driving force for plate tectonics Lithosphere- rigid layer of Earth about 100 km, made of the crust and part of the upper mantle Pangaea- large ancient landmass that was composed of all the continents joined together Plate- a large section of Earth’s oceanic or continental crust and rigid upper mantle that moves around the asthenosphere Plate tectonics- theory that Earth’s crust and upper mantle are broken into plates that float and move around the plasticlike layer of the mantle Seafloor spreading- Jess’s theory that new seafloor is formed when magma is forced upward toward the surface at mid-ocean ridge Convergent boundary- when plates collide with each other Transform boundary- when plates slide pass each other Divergent boundary- plates are moving apart

4. Cornell Notes Title: Plate Tectonics Standards: S6E5. Students will investigate the scientific view of how the earth’s surface is formed. e. Recognize that lithospheric plates constantly move and cause major geological events on the earth’s surface. f. Explain the effects of physical processes (plate tectonics, erosion, deposition, volcanic eruption, gravity) on geological features including oceans (composition, currents, and tides). EQ: What is plate tectonics?

5. The Theory of Plate Tectonics

6. Plate Tectonics The Earth’s lithosphere is divided into plates that move on top of the asthenosphere. Earth’s Major Plates When the water moves beneath the raft, the raft moves with it. When the asthenosphere moves, the lithosphere moves with it… Asthenosphere Lithosphere

7. Types of Plate Boundaries When two plates meet, they form a boundary. There are three types of boundaries 1.Convergent 2.Divergent 3.Transform

8. Convergent Boundaries Two plates push together SUBDUCTION SINKING!Term to know: SUBDUCTION means the crust is SINKING! Three types of convergent boundaries: 1. Oceanic/Oceanic = subduction = TRENCH 2. Oceanic/Continental = TRENCH 3. Continental/Continental = MOUNTAINS **Oceanic crust sinks, **Continental crust rises!!

9. Convergent Collision #1 (Oceanic/Oceanic) (subduction!) Both oceanic plates SINK (subduction!) and form a TRENCH. Magma rises and forms and island arc of volcanoes. Subduction Zone

10. Convergent Collision #2 (Oceanic/Continental) The oceanic plate sinks (subduction!) below the continent and the continental plate slides over the top of the oceanic plate. Forms a TRENCH. Subduction Zone

11. Convergent Collision #3 (Continental/Continental) Both continental plates collide and rise up forming MOUNTAINS. (Ex. Himilayas)

12. Divergent Boundaries Two plates pull apart causing a rift valley in the middle. Sea-floor spreading is created by a divergent boundary. Rift Valley Mid Ocean Ridge

13. Sea Floor Spreading Mid Ocean Ridges – underwater mountain chains that run through the Earth’s Basins Magma rises to the surface and solidifies and new crust forms Older Crust is pushed farther away from the ridge

14. Transform Boundaries Plates slide past each other (Ex. San Andreas Fault)Plates slide past each other (Ex. San Andreas Fault) Causes earthquakes!Causes earthquakes! San Andreas Fault This fence used to line up!!

15. WHY do the plates move? …CONVECTION CURRENTS in the mantle…Hot rock (less dense) rises to the surface, cools (more dense), and sinks back to the mantle. HOT ROCK RISES COOL ROCK SINKS

16. Convection Currents

18. Brain Pop!