0
The Theory of Plate             Tectonics• Is a theory of why and how the continents  move.• The cold, hard, rigid, outer ...
Plates• Continental Crust – Is more buoyant and not as dense as oceanic   crust. It is comprised mainly of granitic rock.•...
The Theory of Plate            Tectonics• The oceanic and continental crust make up  the lithosphere. – Thin outer shell o...
The Theory of Plate             Tectonics• According to the theory, the lithosphere is  broken into plates that ride (or f...
Lithospheric Plate          Boundaries• Some plates move toward each other,  others are moving apart, and some are  simply...
Karaoke Moment
Practice...The wheels on the bus go    round and round    round and round    round and round,The wheels on the bus go     ...
Convection CellsThe mantle of the earthGoes round and round,Round and roundRound and round,The mantle of the earthGoes rou...
Spreading CentersThe convection cells formSpreading centers           Rift ValleySpreading centersSpreading centers,The co...
Subduction ZonesWhen plates come togetherOne slides down,          When plates come togetherOne slides down,              ...
Transform FaultPlates slide past eachother at transform faultsTransform faultsTransform faults,Plates slide past eachother...
Divergent Boundaries• Plates are moving apart from each other• We also term these sites spreading centers.• Form what is k...
Convergent Boundaries• Plates are pushing into neighboring plates.• Usually a subduction zone occurs. That is  when oceani...
Transform Boundaries• Formed when two plates grind past each  other.• Example: – San Andreas Fault
Causes of Plate Motion• Many scientist believe that the movement of  plates is do to convection cells, movement  caused by...
Microplate Terrains Theory– Each terrain has 3 characteristics  • Rocks and fossils unique to it’s terrain  • Major fault ...
Upcoming SlideShare
Loading in...5
×

2.3 theory of plate tectonics

557

Published on

0 Comments
1 Like
Statistics
Notes
  • Be the first to comment

No Downloads
Views
Total Views
557
On Slideshare
0
From Embeds
0
Number of Embeds
1
Actions
Shares
0
Downloads
5
Comments
0
Likes
1
Embeds 0
No embeds

No notes for slide

Transcript of "2.3 theory of plate tectonics"

  1. 1. The Theory of Plate Tectonics• Is a theory of why and how the continents move.• The cold, hard, rigid, outer shell of the earth consist of two types of crust. – Oceanic Crust • Material on the ocean floor – Continental Crust • Crust that makes up land masses
  2. 2. Plates• Continental Crust – Is more buoyant and not as dense as oceanic crust. It is comprised mainly of granitic rock.• Oceanic Crust – Is denser than continental crust because it is crushed by the massive weight of water that is on it. It is mainly comprised of basaltic and sedimentary rock. 2
  3. 3. The Theory of Plate Tectonics• The oceanic and continental crust make up the lithosphere. – Thin outer shell of the earth• Below the lithosphere lies the asthenosphere, a layer of molten rock, that is melted and flows (like putty) under pressure.
  4. 4. The Theory of Plate Tectonics• According to the theory, the lithosphere is broken into plates that ride (or float) on the asthenosphere. – Like blocks of wood floating on water.
  5. 5. Lithospheric Plate Boundaries• Some plates move toward each other, others are moving apart, and some are simply sliding past one another.• This constant movement is what has created our earth’s major surface. – Mountain Ranges – Deep-ocean Trenches
  6. 6. Karaoke Moment
  7. 7. 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.
  8. 8. Convection CellsThe mantle of the earthGoes round and round,Round and roundRound and round,The mantle of the earthGoes round and roundAll underground
  9. 9. Spreading CentersThe convection cells formSpreading centers Rift ValleySpreading centersSpreading centers,The convection cells formSpreading centersCreating rift valleys
  10. 10. Subduction ZonesWhen plates come togetherOne slides down, When plates come togetherOne slides down, One slides down,One slides down. We call it a subduction zone.
  11. 11. Transform FaultPlates slide past eachother at transform faultsTransform faultsTransform faults,Plates slide past eachother at transform faultsand we live next to one! San Andreas Fault
  12. 12. 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.
  13. 13. 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
  14. 14. Transform Boundaries• Formed when two plates grind past each other.• Example: – San Andreas Fault
  15. 15. Causes of Plate Motion• Many scientist believe that the movement of plates is do to convection cells, movement caused by hot and cooler spots in the mantle. So, the mantle is churning.
  16. 16. Microplate Terrains Theory– Each terrain has 3 characteristics • Rocks and fossils unique to it’s terrain • Major fault at every boundary • Different magnetic properties 16
  1. A particular slide catching your eye?

    Clipping is a handy way to collect important slides you want to go back to later.

×