1. Monday 3/4 2. What type of material makes up the earth’s core? Iron and nickel Inner core solid Outer core liquid

2. Tue 3/5 3. What is the lithosphere? Includes the crust and upper mantle.

3. Wed 3/6 4.Who was Alfred Wegener? He proposed the theory of continental drift

4. Thur 3/7 5. What is the asthenosphere? is the ductile part of the earth just below the lithosphere, “plasticity”.

5. Fri 3/8 6. Label the layers. A.Crust B.Mantle C.Outer core D.Inner core E.Lithosphere F.asthenosphere

8. Monday 3/18 7. What are the primary chemical components of the crust, mantle, and core? Crust - oxygen and silicon, known as silicates Mantle – same as crust with heavier elements Core - very dense materials, primarily iron and nickel.

9. Tue 3/19 8. What is the state of matter of the lithosphere, and how can its location be described? Solid Includes the crust and upper mantle

10. Wed 3/20 9. What does the theory of plate tectonics explain ? How earth’s plates form, move, and interact.

12. Thursday 3/21 9. What are the 3 types of plate boundaries? Convergent – O> <C Divergent Transform

13. Monday 10. What causes the plates to move? Convection currents created by heat

14. Tue 3/26 11. What happens when 2 continental plates collide? Mountains are created

15. Wed 3/27 12. Name the Plates. 1.Pacific 2.N.A. 3.S.A. 1. 2. 3.

16. Mon 4/1 13. Why is Pangaea not a perfect fit? Weathering and Erosion Sea level change

17. Wed 4/3 14. What two factors keep the planets in their orbits? Gravity Inertia

20. both gravity and inertia work together to keep planets in orbit around the sun -inertia makes a planet travel in a straight line -by definition, inertia is the tendency of a moving object to stay in a straight line or a stationary object to remain in place -however, the power of the sun's gravity pulls the planets toward the sun -the sun's gravity pulls the planets while their inertia keeps them moving forward in an elliptical orbit around the sun -the strength of gravity in our solar system depends on both the masses of the celestial objects and the distance between them -gravity helps to explain the tides on earth -without inertia, a planet would be pulled into the sun

21. Ch. 16 voc 1.Geocentric system 2.Heliocentric system 3.Solar system 4.Ellipse 5.Inertia 6.Gravity 7.Rotation 8.Revolution 9.Mercury 10.Venus 11.Earth 12.Mars 13.Magellan 14.Gas giants 15. Jupiter 16. Saturn 17. Uranus 18. Neptune 19. Pluto 20. Comet 21. Asteroid 22. Asteroid belt 23. Meteoroid 24. Meteor 25. meteorite

22. 5 cm

23. 1. Geocentric system The idea that earth was the center, the sun and planet revolved around earth 2. Heliocentric The idea that the sun is at the center of a system of planets. 3. Solar system all objects that orbit the “sun”.

24. 4. Ellipse An elongated circle, or oval shape. 5. inertia The tendency of a moving object to continue in a straight line or a stationary object to remain in place. 6. Gravity This force attracts all objects towards on another. 7. rotation The spinning motion of a planet about its axis. 8. revolution The movement of a planet around the sun.

25. 9. Mercury Planet closest to the sun, no atmosphere, hot. 10. Venus This planet is so similar in size to Earth that it is sometimes called Earth’s twin. 11. Earth 3 rd planet from the sun, supports life. 12. Mars This planet is called the “red planet” because it has a slightly reddish tinge when you see it in the sky.

26. Pre Ap 1.B 2.B 3.B 4.D 5.C 6.A 7.C 8.B 9.A 10.D 11.D 12.A 13.A 14.B 15.A 16.D 17.D 18.D 19.B 20.C 1.95/96 2.90/93 3.85/89 4.80/85 5.75/81 6.70/78 7.65/74 8.60/70 9.55/66 RETAKE WED MORNING

27. 195/97 290/93 385/90 480/86 575/83 670/79 765/76 860/72 955/70 1050/65 retake wed morn. 1145/62 1240/58 1335/55 1430/ 51 1525/48 1620/44 1715/41 1.B 2.B 3.B 4.D 5.C 6.A 7.C 8.B 9.A 10.D 11.D 12.A 13.A 14.B 15.A 16.D 17.D 18.D 19.B 20.C MOD 1 C 2 B 3 C 4 A 5 B 6 A 7 B 8 C 9 A 10 B 11 A 12 B 13 B 14 C 15 B 16 B 17 C 18 B 19 C 20 B

28. 1 C 2 B 3 C 4 A 5 B 6 A 7 B 8 C 9 A 10 B 11 A 12 B 13 B 14 C 15 B 16 B 17 C 18 B 19 C 20 B 195/97 290/93 385/90 480/86 575/83 670/79 765/76 860/72 955/70

29. Strack STAAR Testing Bell Schedule April 2 and 3, 2013 Pds. 1-4:7 th and 8 th Grade Testing 6 th Grade Silent Bell Schedule (No locker stops until 5 th period) Pds. 5-7: Regular Bell Schedule PERIOD 1: 9:00 – 9:57 PERIOD 2: 10:02 – 10:58 PERIOD 3: 11:03 – 12:00 PERIOD 4: 12:00 – 12:25 A Lunch 6 th Grade 12:30– 12:55 B Lunch 7 th Grade 1:00 –1:25 C Lunch 8 th Grade (7 th returns to testing rooms) PERIOD 5:1:30–2:15 PERIOD 6: 2:20–3:05 PERIOD 7: 3:10 –3:55

30. 1. What are the relative positions of the celestial bodies that make up the solar system? 2. How do periods of rotation, periods of revolution, and shape of orbital paths di!er between celestial bodies of our solar system? 3. What are the physical properties of each of the following: the Sun, planets, moons, asteroids, meteors, and comets? 4. How is Earth’s moon similar and dissimilar to the characteristics and motion of the Galilean moons?

32. Periods Monday 3/25 1.Turn in warm ups 2.Lab 3.Worksheet map plate tectonics p. 355 Tue 3/26 1.Turn in worksheet 2.Review for test Wed 1. Test CCA layers of the earth and plate tectonics

34. Scotia Plate

36. Monday 3/18 1.Worksheet 10-1 p. 326 cw hw 2.Finish movie Tue 3/19 1.Turn in ws 2.Work on voc booklet 3.Draw page 359 on last page of booklet Wed 3/20 1.voc. booklet due end of period 2.Worksheet 11-1 cw hw Thur 3/21 1.Turn in 11-1 ws 2.Turn in warm ups 3.Work on worksheet overview plate tectonics due mon 4.video

37. Monday 3/18 1.Worksheet 10-1 p. 326 cw hw 2.Finish movie Tue 3/19 1.Turn in ws 2.Work on voc booklet 3.Draw page 359 on last page of booklet Wed 3/20 1.voc. booklet due end of period 2.Worksheet 11-1 cw hw Thur 3/21 1. Voc book 2.11-1 ws cw 3.Turn in warm ups 4. video

38. 1. Earth’s layers can be identi!ed using two properties: (1) basic chemical composition, and (2) state of matter. 2. As Earth cooled and formed a planet, the less dense elements of the crust and mantle separated, forming layers around the dense core. 3. The crust and mantle are composed primarily of the elements, oxygen and silicon, known as silicates. Silicates of the mantle contain heavier elements, making them more dense than those found in the crust. The core is composed of the most dense materials, primarily iron and nickel. 4. The outer core is in the liquid state and the inner core is in the solid state of matter. 5. The lithosphere is found in the solid state and is a layer that contains all of the crust and a little of the upper mantle. 6. The asthenosphere is a shallow layer of the upper mantle and lies directly below the lithosphere. The state of matter of the asthenosphere is a solid; however, it has “plasticity” that allows it to “flow. 7. When constructing a model of the layers of Earth, chemical composition, state of matter, and thickness of each layer should be considered.

39. What properties are utilized to identify and define the layers of Earth? Why does Earth have layers? What are the primary chemical components of the crust, mantle, and core? What is the state of matter of the outer core and the inner core? What is the state of matter of the lithosphere, and how can its location be described? What is the state of matter of the asthenosphere, and how can its location be described? What does “plasticity” have to do with the asthenosphere’s state of matter? What should be considered when developing a model of Earth’s layers

42. Earth’s layers 328 Inner core 328 Outer core 328 mantle329 Crust 329 Asthenosphere - The solid layer with plasticity in the upper mantle that is located just below the lithosphere; lithospheric plates “Float” and move on this layer Lithosphere 354 Alfred Wagener 354 Pangaea 355 Plate tectonics 355 Theory of plate tectonics 356 Plate boundaries 356 Earthquake 358 Stress 358 Shearing 359 Tension 359 Compression 359 Fault 360

43. Earth’s layers ( draw and label layers) earth’s interior is divided into layers.

44. Inner core ( draw and label) solid iron and nickel, pressure to great to melt.

45. Outer core (draw layers) liquid metal, iron and nickel

46. Mantle -The solid layer of Earth between the crust and the core; made of dense silicates

47. Crust The thin solid outermost layer of Earth; made of less dense silicates and is continental (landmasses) or oceanic (ocean bottoms)

48. Asthenosphere The solid layer with plasticity in the upper mantle that is located just below the lithosphere; lithospheric plates “Float” and move on this layer

49. Lithosphere -The cool, rigid, outermost layer of Earth consists of the crust and the uppermost part of the mantle; pieces of this layer are called lithospheric plates

50. asthenosphere The solid layer with plasticity in the upper mantle that is located just below the lithosphere; lithospheric plates “Float” and move on this layer

51. Alfred Wagener - the scientist who theorized continental drift, plate tectonics, and Pangae

52. Pangaea – alfred wageners super continent 150 mya

53. Plate tectonics – study how plates move and features on earth.

54. Theory of plate tectonics -states that the earth’s crust is broken into plates that are constantly moving.

56. Plate boundaries - are found at the edge of the lithospheric plates and are of three types, convergent, divergent and transform.

57. Earthquake - is the result of a sudden release of energy in the Earth's crust that creates seismic waves.

58. Stress A force that acts on rock to change its shape or volume.

59. shearing Side to side movement

60. Tension Pulls the crust apart

61. compression Squeezes rock together

62. Fault Small movements of the earths crust