
Types of Plate Boundary
Presentation
•
Science
•
9th - 10th Grade
•
Hard
Jason Morvan
Used 17+ times
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10 Slides • 0 Questions
1
Types of Tectonic Plate Boundary
by Jason Morvan
2
Transform Boundaries
Plates slide across each other
No new boundary is made or destroyed
Friction causes a build-up of pressure
Eventually, the pressure causes a jolt (earthquake)
May occur between any type of plate
Cause shallow-focus earthquakes (less than 70km deep)
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Convergent Boundaries
Occur when plates colliding head-on
Generate the most violent earthquakes
Can cause mountain ranges, volcanoes, or trenches to form
The denser plate will disappear under the less-dense one (subduction zone)
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Continent to Continent Collision
Both plates have similar densities, so no subduction occurs
Instead, both plates push on each other, causing mountain ranges (the Himalayas are an example)
5
Ocean to Continent Collision
Oceanic plates are denser, so always disappear underneath the continental plate (known as subduction)
The line where the plates meet is called an ocean trench
Can produce mountain ranges with volcanoes
As oceanic plate subducts and melts, it can be forced into the volcano above
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Ocean to Ocean Collisions
The older crust will be denser, so will disappear under the younger plate
A deep-ocean trench is formed
As the denser plate gets hotter in the mantle, it melts and may be forced up, creating a line of undersea volcanoes, called an island arc (Japan and Indonesia are example where this has occurred)
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Australian Earthquakes
The continent of Australia is in the middle of the Australian tectonic plate
New Zealand is on the edge of the Australian and Pacific plates
New Zealand is more likely to have large earthquakes (NZ's largest recorded earthquake was 8.2 on the Richter scale; Au's largest ever was 6.6)
Australia still has about 100 earthquakes (3.0 or larger) every year!
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Tsunamis Caused by Earthquakes or Volcanoes
Earthquakes or volcanoes under the seabed cause water to be shifted
This water travels at about 800km/hr through the deep ocean
As it approaches shallow water and land, it slows down, but increases in height
Tsunami means "harbour wave" in Japanese
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Diverging Boundaries
Caused by plates spreading apart
Can occur in the middle of the ocean or even in the middle of a continent
Magma from underneath the crust rises up and pushes on the plate
The continental plate is thinned out and a rift valley is formed
It is thought that Pangaea broke apart due to diverging plates
Eventually, the gap between continental land masses grows large enough for water to flow in, forming a lake, sea, and eventually, an ocean
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Creating New Land
In the same way that converging boundaries can destroy plates (at a subduction zone), diverging boundaries can create new plates
Magma forces up and pushes the plates apart, forming a mid-ocean ridge
As this magma hardens, it becomes part of the tectonic plate
Continental plates tend to be much older than oceanic plates, because the denser plates melt as they subduct
Types of Tectonic Plate Boundary
by Jason Morvan
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