1. Plate Tectonics 7 th Grade Science

2. Lesson 1 Earthquake- vibrations in the earth caused by sudden release of energy, as a result of the movement of rocks along a fault Earthquake- vibrations in the earth caused by sudden release of energy, as a result of the movement of rocks along a fault Seismologist- scientist who studies earthquakes Seismologist- scientist who studies earthquakes

3. Lesson 2 Earthquake Waves Earthquake Waves P-Wave: primary wave, first and compressional (back and forth) P-Wave: primary wave, first and compressional (back and forth) S-Wave: secondary, second and moves at right angles, much rougher S-Wave: secondary, second and moves at right angles, much rougher Surface Waves: Elliptical and back and forth on surface of earth, most destructive Surface Waves: Elliptical and back and forth on surface of earth, most destructive

4. Lesson 3 Seismogram- paper that records earthquake Seismogram- paper that records earthquake Seismograph- device that measures an earthquake’s intensity Seismograph- device that measures an earthquake’s intensity Epicenter – imaginary point on earth that sits on top of the focus Epicenter – imaginary point on earth that sits on top of the focus Focus – where the earthquake begins inside the earth Focus – where the earthquake begins inside the earth

5. Earthquake Diagram

6. Lesson 4 Plate Boundary-pieces of broken lithosphere meet, 3 types Convergent (collide), Divergent (divide) and transform (slide) Plate Boundary-pieces of broken lithosphere meet, 3 types Convergent (collide), Divergent (divide) and transform (slide) Ring of Fire-encircles the Pacific Ocean, an area of volcanic and earthquake activity Ring of Fire-encircles the Pacific Ocean, an area of volcanic and earthquake activity Magnitude- measure of total amount of energy released in an earthquake, each interval 32 times more energy is released Magnitude- measure of total amount of energy released in an earthquake, each interval 32 times more energy is released Intensity- measure of damage done during an earthquake Intensity- measure of damage done during an earthquake

7. Lessons 1-4 Challenge Words Liquefaction: strength and stiffness of soil is reduced by earthquake shaking, occurs in saturated soils and allows soil particles to move (think of liquid vs. solid) Liquefaction: strength and stiffness of soil is reduced by earthquake shaking, occurs in saturated soils and allows soil particles to move (think of liquid vs. solid) Lithosphere: crust and uppermost mantle, where earthquakes occur Lithosphere: crust and uppermost mantle, where earthquakes occur Subduction Zone: 2 lithospheric plates come together Subduction Zone: 2 lithospheric plates come together

8. Lesson 5 Parts of the Earth (inside to outside)-think of an apple Parts of the Earth (inside to outside)-think of an apple Inner Core/like the seeds of an apple Inner Core/like the seeds of an apple Outer Core/pocket that holds the seeds Outer Core/pocket that holds the seeds Mantle/meaty part of the apple-what you eat Mantle/meaty part of the apple-what you eat Lithosphere/bite out of the apple-upp.mantle/crust or a plate Lithosphere/bite out of the apple-upp.mantle/crust or a plate Crust/skin of the apple Crust/skin of the apple

9. Lesson 6 Lithosphere: Cool, solid outer shell of earth which is made of Crust and Upper Mantle and makes up our plates Lithosphere: Cool, solid outer shell of earth which is made of Crust and Upper Mantle and makes up our plates Asthenosphere: layer of mantle directly below the lithosphere and allows the lithosphere to move. Asthenosphere: layer of mantle directly below the lithosphere and allows the lithosphere to move. Mid-Ocean Ridge: A mountainlike landform that develops when plates separate and new ocean lithosphere forms Mid-Ocean Ridge: A mountainlike landform that develops when plates separate and new ocean lithosphere forms Subduction: The movement of a tectonic plate beneath another plate Ex. Oceanic lithosphere is more dense and subducts beneath the Continental lithosphere Subduction: The movement of a tectonic plate beneath another plate Ex. Oceanic lithosphere is more dense and subducts beneath the Continental lithosphere Seafloor Spreading: Mid-Ocean Ridge where magma is being pushed out of the crust creating new rock Ex. A Divergent Boundary like in the Atlantic Ocean between N.America and Europe/Asia Seafloor Spreading: Mid-Ocean Ridge where magma is being pushed out of the crust creating new rock Ex. A Divergent Boundary like in the Atlantic Ocean between N.America and Europe/Asia

10. Lesson 7 Brittle: describes objects that break easily when force is applied to them Brittle: describes objects that break easily when force is applied to them Ductile: describes objects that bend, stretch, or flow when a force is applied to them Ductile: describes objects that bend, stretch, or flow when a force is applied to them Fault: a fracture in bedrock, along which blocks of rock on opposite sides of the fracture move Ex. San Andreas Fault, California Fault: a fracture in bedrock, along which blocks of rock on opposite sides of the fracture move Ex. San Andreas Fault, California Plate Tectonics: Theory that lithosphere is broken into segments/plates that float on the asthenosphere and is associated with earthquakes, and volcanic activity. Plate Tectonics: Theory that lithosphere is broken into segments/plates that float on the asthenosphere and is associated with earthquakes, and volcanic activity.

11. Lesson 8 Convection in the Mantle: the heat from our core travels to the Mantle and rises since it is less dense than the cooler material at the top of the mantle. The cooler material is more dense so it sinks. This cycle repeats itself and is known as a convection current. (Think of our Boiling pot of water or our Convection experiment with the bottle and candle. ) This process drives our plate movement. Convection in the Mantle: the heat from our core travels to the Mantle and rises since it is less dense than the cooler material at the top of the mantle. The cooler material is more dense so it sinks. This cycle repeats itself and is known as a convection current. (Think of our Boiling pot of water or our Convection experiment with the bottle and candle. ) This process drives our plate movement.

12. Lessons 9 – 12 (Our destructive and constructive Volcanoes) Volcano – a mountain with a crater or vent in which molten material, gas, and ash can escape Volcano – a mountain with a crater or vent in which molten material, gas, and ash can escape Types of: Types of: Shield: has gently sloping sides and gentler eruptions ex. Mt. Kilauea, Hawaii Shield: has gently sloping sides and gentler eruptions ex. Mt. Kilauea, Hawaii Cinder-cone: Steep mountain with large cone like crater at the time, can have great eruptions ex. Paricutin in Mexico Cinder-cone: Steep mountain with large cone like crater at the time, can have great eruptions ex. Paricutin in Mexico Composite or Stratovolcano: Made of alternating layers of lava or ash, can have major eruptions, Ex. Mt. Pinatubo in the Phillippines Composite or Stratovolcano: Made of alternating layers of lava or ash, can have major eruptions, Ex. Mt. Pinatubo in the Phillippines

13. Volcano types

14. More Vocabulary Volcanic Ash/tephra: Trapped gases from a volcano emit these tiny fragments of volcanic remains/glass into the atmosphere Volcanic Ash/tephra: Trapped gases from a volcano emit these tiny fragments of volcanic remains/glass into the atmosphere Magma: Molten material beneath the earth’s surface Magma: Molten material beneath the earth’s surface Lava: Molten material on the earth’s surface Lava: Molten material on the earth’s surface Hot Ash Cloud: the pressure released during a volcanic eruption can produce these clouds due to density differences between ash and air and convecton Hot Ash Cloud: the pressure released during a volcanic eruption can produce these clouds due to density differences between ash and air and convecton

16. Instruments used to study Volcanoes Seismograph Seismograph Gas Sensors Gas Sensors Tiltmeter Tiltmeter