Download presentation
Published byReynold Summers Modified over 9 years ago
1
Major Geological Events Caused by Plate Tectonics
2
Types of Boundaries Divergent Plates move apart Convergent
Plates come together Transform Plates slide horizontally past each other
3
DIVERGENT {PLATE} BOUNDARY
What are DIVERGENT plates? They are plates that move in the opposite direction of each. How do DIVERGENT plate boundaries work? They pull apart allowing magma to ooze through the cracks to the surface of the sea floors What do DIVERGENT plate boundaries form? New Crust Form mountain ranges on the sea floor.
4
CONVERGENT {PLATE} BOUNDARY
What are CONVERGENT plates? They are plates that COLLIDE with each other How do CONVERGENT plate boundaries work? The continental crust {what we live on} and the oceanic crust {under the sea} collide. The oceanic crust {more dense} sinks below the continental crust {less dense}. What do CONVERGENT plate boundaries form? Major Earthquakes Volcanic Mountains Deep sea trenches
5
TRANSFORM {PLATE} BOUNDARY
What are TRANSFORM plates? The action of two plates that are sliding past each other How do TRANSFORM plate boundaries work? These plates sliding past each other horizontally cause large amounts of energy to build up. What do TRANSFORM plate boundaries form? Tsunami Major Earthquakes Faults
6
Subduction Result of convergent boundary
A more dense plate slides under a less dense plate and sinks into the mantle. Features include: Oceanic-Oceanic = Trenches Oceanic-Continental = Mountain Ranges
7
PLATE TECTONICS A theory that explains the movement of continents Massive Slab of rock Irregularly shaped Located and Float on the Lithosphere Move around Earth by circulating CONVECTION CURRENTS {hot liquid rises and cold liquid sinks, moves in a circular motion, the energy gets transferred} Move only a few centimeters each year Most of the events happen near the boundaries
8
Trench - a depression in the ground that is generally deeper than it is wide
9
Fault Lines – break in the Earth’s crust
10
Transform Boundary San Andreas Fault Line
11
Rift Valley – lowland between several highlands or mountain ranges caused
by a fault
12
Rift Valley Divergent Structure
Divergent Structure
13
Mid–Ocean Ridge (Location of Sea Floor Spreading)
14
Sea Floor Spreading (Mid-Ocean Ridge)
Younger Older Older Divergent Structure
16
Transform Boundary Oceanic-Oceanic Land Feature – Fault Line
17
Volcanoes
18
Earthquakes – All Boundaries
19
Subduction Examples
20
Oceanic-Oceanic convergence
Convergent Boundary Oceanic-Oceanic Land Features – Trench and Island Arc Oceanic-Oceanic convergence
21
Oceanic-Continental convergence
Convergent Boundary Oceanic-Continental Land Features – Trench and Volcanic Arc (Volcanic Mountains) Oceanic-Continental convergence
22
Continental-Continental convergence
Convergent Boundary Continental-Continental Land Features – Folded Mountains Continental-Continental convergence
23
Mountain Ranges
24
Transform Boundary Continental-Continental Land Features – Fault Line
Aerial view of San Andreas Fault in the Carrizo Plain, self-made, Nov 16, 2007, I. Kluft,
25
Putting It All Together
26
Plate Movement
Similar presentations
© 2025 SlidePlayer.com. Inc.
All rights reserved.