Presentation is loading. Please wait.

Presentation is loading. Please wait.

Warm Up 1) Take out your Vocabulary Chart and make sure it is complete so I can come around and give you credit.

Similar presentations


Presentation on theme: "Warm Up 1) Take out your Vocabulary Chart and make sure it is complete so I can come around and give you credit."— Presentation transcript:

1 Warm Up 1) Take out your Vocabulary Chart and make sure it is complete so I can come around and give you credit.

2 Plate Tectonics Chapter 25 Section 1 Earth’s Internal Processes
Earth’s surface is broken into large pieces called plates. These plates move slowly, floating on the lower layers

3

4 Plate Tectonics Chapter 25 Section 1 Earth’s Internal Processes
Earth’s surface is broken into large pieces called plates. These plates move slowly, floating on the lower layers 2 types of plates 1. Continental plates 2. Oceanic plates Made of thick crust that is not very dense Made of thin crust that is more dense than Continental crust

5 Continental vs. Oceanic Crust
Notice that the Oceanic Crust is thinner than the Continental crust

6 Plate Tectonics Chapter 25 Section 1 Earth’s Internal Processes
Earth’s surface is broken into large pieces called plates. These plates move slowly, floating on the lower layers 2 types of plates 1. Continental plates 2. Oceanic plates Plate Boundaries -3 types 1. Convergent 2. Divergent 3. Transform Made of thick crust that is not very dense Made of thin crust that is more denser Area where two plates interact Area where two plates collide Area where two plates move apart Area where two plates slide past each other

7 Identify the boundary type.
Divergent Convergent Transform

8 Chapter 25 Section 1 Earth’s Internal Processes
Notes from video Divergent boundaries -As plates move apart from each other, magma rises up to fill in the gap and forms new rock -When happens on ocean floor a Mid Ocean Ridge forms -When happens on continent a rift forms -Rocks are youngest closest to the divergent boundary Convergent boundaries Three types: 1. Continental-Continental collision 2. Continental-Oceanic collisions Oceanic-Oceanic -When continental crust pushes against continental crust, mountains form. -When continental crust pushes against oceanic crust, oceanic crust sinks under the continental crust. This is called subduction. A trench and volcanoes form. -When oceanic crust pushes against oceanic crust, one plate sinks and very deep trenches are formed -Strange life forms are found in these trenches

9 Transform boundaries Convection currents
Chapter 25 Section 1 Earth’s Internal Processes Transform boundaries Convection currents When plates slide past each other, Earthquakes occur San Francisco is an example. Motion of plates is caused by motion of magma called convection currents

10

11

12 Transform boundaries Convection currents
Chapter 25 Section 1 Earth’s Internal Processes Transform boundaries Convection currents When plates slide past each other, Earthquakes occur San Francisco is an example. Motion of plates is caused by motion of magma called convection currents Draw a picture of convection currents Notes are finished for section 1 Reread all of your notes

13


Download ppt "Warm Up 1) Take out your Vocabulary Chart and make sure it is complete so I can come around and give you credit."

Similar presentations


Ads by Google