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INTERNALS DYNAMICS
Interior of the earth

Crust
Mantel
Outer core
Inner core
Solid
5km
Lithosphere
Upper
Lower
Solid
solid rock
Melte
2.900km
lithosphere
asthensophere
mesosphere
liquid
2,890/5,150 km
Solid
5,150/6,378 km
granite
sedimentary rocks
metamorphic rocks
molten iron
minerals
other semi-solid rocks that will still flow under pressure
iron
nickel
oxygen
sulfur
iron
nickel
The movement of plates
Oceanic crust
Continental crust
Plate margins
underneath the oceans
can be subducted
It is denser than continental crust
under land masses or continents
older than oceanic crust
less often destroyed
Earthquakes are found along all types of plate margins
Volcanoes occur at constructive and destructive plate margins
Convergent Boundaries
Divergent Boundaries
Transform Boundaries
two plates collide
crust is destroyed
oceanic-oceanic
continental+continental
plates that separate
creates new crust
earthquakes
volcanoes
plates slide horizontally
collide they get stuck
rock breaking
earthquakes
Information
- Description
- Flowchart on Science mind map, created by Noa Rodriguez Gazquez on 27/04/2021.
- Created by
- Noa Rodriguez Gazquez · Apr 2021
- Updated
- May 2, 2021
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