1. The SEE, HEAR, and
DO Approach to
AG Earth Science!

2. CULTURE CAMP

4. Try Again

5. CST
PAC
TPE
T BTSA
FACT
API

6. TPR

7. TOTAL
PHYSICAL
RESPONSE

8. HOW LEARNING OCCURS
0 25 50 75 100
HEAR
SEE
SEE AND HEAR
SEE HEAR SAY DO

9. MY ADVICE
• PICTURES everywhere, share your own
• REPEAT yourself constantly
• have students SAY info back to you
• do DEMOS as much as possible
• short and meaningful VIDEOS
• PLAY games
• let students DO activities

10. MY ADVICE
• PICTURES everywhere, share your own
• REPEAT yourself constantly
• have students SAY info back to you
• do DEMOS as much as possible
• short and meaningful VIDEOS
• PLAY games
• let students DO activities

11. MY ADVICE
• PICTURES everywhere, share your own
• REPEAT yourself constantly
• have students SAY info back to you
• do DEMOS as much as possible
• short and meaningful VIDEOS
• PLAY games
• let students DO activities

12. MY ADVICE
• PICTURES everywhere, share your own
• REPEAT yourself constantly
• have students SAY info back to you
• do DEMOS as much as possible
• short and meaningful VIDEOS
• PLAY games
• let students DO activities

13. MY ADVICE
• PICTURES everywhere, share your own
• REPEAT yourself constantly
• have students SAY info back to you
• do DEMOS as much as possible
• short and meaningful VIDEOS
• PLAY games
• let students DO activities

14. MY ADVICE
• PICTURES everywhere, share your own
• REPEAT yourself constantly
• have students SAY info back to you
• do DEMOS as much as possible
• short and meaningful VIDEOS
• PLAY games
• let students DO activities

15. MY ADVICE
• PICTURES everywhere, share your own
• REPEAT yourself constantly
• have students SAY info back to you
• do DEMOS as much as possible
• short and meaningful VIDEOS
• PLAY games
• let students DO activities

16. LET’S TRY A FEW

18. Planet Earth

19. Solar System

20. Milky Way Galaxy

21. Milky Way Galaxy
Sun
Alpha Centari

22. A Spot in the Sky

23. UNDERSTANDING
OUR EARTH

24. THE EARTH IS LIKE A
PEACH

25. PLATE TECTONICS

26. LET’S GET OUR PLATES
ON!

27. CONCLUSIONS
move apart
come together
slide past each other

28. Divergent Boundaries
• Plates are moving apart from each other
• We also term these sites spreading centers.
• Form what is known as a rift valley.
It is at divergent plate
boundaries where new
crust is created.

29. Pillow Basalts

30. Convergent Boundaries
• Plates are pushing into neighboring plates.
• Usually a subduction zone occurs. That is
when oceanic crust crashes into and slides
under continental crust.
• 3 convergent boundaries can occur:
–continental/oceanic crust collision
–oceanic/oceanic collision
–continental/continental collision

31. Transform Boundaries
• Formed when two plates grind past each
other.
• Example:
–San Andreas Fault

32. Deep Accretionary Forearc Volcanic
Ocean Wedge Basin Arc
Trench (1) (2) (3) (4)
1 2 3 4

33. continent is created by the subduction of
oceanic crust under oceanic crust
Japan
Eurasian Plate Pacific Plate

34. Indo-Australia Eurasia
Plate Plate
Himalayas
India Tibetan
plateau
Suture

35. Karaoke Moment

36. Practice...
The wheels on the bus go
round and round
round and round
round and round,
The wheels on the bus go
round and round
all through the town.

37. Convection Cells
The mantle of the earth
Goes round and round,
Round and round
Round and round,
The mantle of the earth
Goes round and round
All underground

38. Spreading Centers
The convection cells form
Spreading centers Rift Valley
Spreading centers
Spreading centers,
The convection cells form
Spreading centers
Creating rift valleys

39. Subduction Zones
When plates come together
One slides down, When plates come together
One slides down, One slides down,
One slides down. We call it a subduction zone.

40. Transform Fault
Plates slide past each
other at transform faults
Transform faults
Transform faults,
Plates slide past each
other at transform faults
and we live next to one!
S a n A n d r e a s F a u l t

41. CRUSTAL
DEFORMATION

42. Brittle Deformation

43. Ductile Deformation

46. UNLOADING AND
EXFOLIATION
Uplifting and fracturing of exterior layers of rock

47. IN A DOORWAY

48. EXFOLIATION

51. FAULTING

52. TYPES OF FAULTS
• Normal fault: hanging wall moves down
relative to the footwall along divergent
boundary
• Reverse fault: compression causes the
hanging wall to move up relative to the
footwall
• Thrust fault: fault plane is a low angle or
nearly horizontal & hanging wall is pushed
up over rock
• Strike-slip fault: rock on either side of the
fault plane slides horizontally at transform
boundaries

53. I SCRATCH YOUR
BACK,YOU SCRATCH
MINE

54. VOLCANOES

55. BUILD THEM
DRY ICE AND WATER
BAKING SODA AND VINEGAR
DIET COKE AND MENTOS
55

57. 57

58. 58

59. 59

60. Igloo Video Clip
60

61. VOLCANO VIDEO

62. BRING IN THE ROCKS

69. EARTHQUAKES

70. P Waves
–Primary Waves (P waves): move fastest and are recorded first
• Can travel through solid & liquid
• Compression waves- cause the rock particles to move together & apart along
the wave direction

71. S Waves
– Secondary Waves (S waves): second to be
recorded
• Travel only through solid material: cannot be detected
on the side of the earth opposite the epicenter…Why?
Can’t go through the liquid of the earth’s outer core!
• Shear waves- cause rock particles to move at right
angles to the wave direction
71

72. REVIEW AND ASSESSMENT

73. Types &
Mountain Earthquakes Recording
Results of Potpourri
Formations & Plates Earthquakes
Stress
100 pt 100 pt 100 pt 100 pt 100 pt
200 pt 200 pt 200pt 200 pt 200 pt
300 pt 300 pt 300 pt 300 pt 300 pt
400 pt 400 pt 400 pt 400 pt 400 pt
500 pt 500 pt 500 pt 500 pt 500 pt

74. STUMP THE TEACHER

75. PICTURE WORTH A
1000 WORDS

77. POWERPOINT
KARAOKE

78. RESOURCES

79. Questions
Concerns
Comments

80. Joey Silva
jsilva@mychawanakee.org
209.201.9171
funwithearthscience
.wikispaces.com