Lab 4: The movement of the Earth’s Lithospheric Plates.

10
Lab 4: The movement of the Earth’s Lithospheric Plates

Transcript of Lab 4: The movement of the Earth’s Lithospheric Plates.

Page 1: Lab 4: The movement of the Earth’s Lithospheric Plates.

Lab 4: The

movement of the Earth’s

Lithospheric Plates

Page 2: Lab 4: The movement of the Earth’s Lithospheric Plates.

•One Plate Subducts•A trench forms above the subduction

zone in water•A volcanic island arc forms on the

plate that is not subducted

Ocean – Ocean Convergence

Page 3: Lab 4: The movement of the Earth’s Lithospheric Plates.

•Ocean plate is subducted below continent.•A trench forms above the subduction zone

in water•A volcanic mountain chain forms on land

Ocean – continent Convergence

Page 4: Lab 4: The movement of the Earth’s Lithospheric Plates.

•No subduction because continents are less dense than the mantle

•Continents collide and fold up (crunch) to form mountains

continent – continent Convergence

Page 5: Lab 4: The movement of the Earth’s Lithospheric Plates.

Ocean – Continent Convergence

1. A. When an ocean plate converges with a

continental plate, what happens? (Which plate subducts?) Explain.

B. What is a subduction zone?

C. What feature is found on the earth directly above the subduction zone?

D. What feature forms on land? Explain.

Page 6: Lab 4: The movement of the Earth’s Lithospheric Plates.

Ocean – ocean Convergence

2.A. When two ocean plates collide, what happens?

B. What feature is found on the earth’s surface directly above the

subduction zone?

C. What feature forms on the ocean plate

that is not subducted? Explain.

Page 7: Lab 4: The movement of the Earth’s Lithospheric Plates.

Continent– Continent Convergence

3.A. When two continents collide, what happens?

B. What feature forms on the earth’s surface because of the collision?

C. Why don’t continents go down at the

subduction zones?

Page 8: Lab 4: The movement of the Earth’s Lithospheric Plates.

Lab 4: VOCABULA

RY

Page 9: Lab 4: The movement of the Earth’s Lithospheric Plates.

11. Continental CrustThicker, less dense, older lithospheric

plate

49. Oceanic CrustThinner, more dense, younger

lithospheric plate

Page 10: Lab 4: The movement of the Earth’s Lithospheric Plates.

15. Continent-Continent Collision Zones

Areas where two plates of the same density (continental crust) move toward each other

and collide

46. Subduction

The movement when one plate (oceanic crust) dives below another plate into the

mantle