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Geography plate margins
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Plate Margins
3 main types of plate margins (most common)
Constructive also known as divergent
Conservative also known as transform
Destructive also known as convergent

Constructive
Lava from mantle-
Convection currents in the magma drive plate tectonics. Heat generated from the radioactive decay of elements deep in the interior of the Earth creates magma (molten rock) in the aesthenosphere. The aesthenosphere (70 ~ 250 km) is part of the mantle, the middle sphere of the Earth that extends to 2900 km.
Crust-
The crust is the outer layer of the earth. It is a thin layer between 0-60 km thick. The crust is the solid rock layer upon which we live.
Conservative

https://www.youtube.com/watch?v=Mkm-vqkOyUM (Einbetten)
Destructive

Continental crust-
The continental crust is the layer of igneous, sedimentary, and metamorphic rocks which forms the continents
Lithosphere-
The lithosphere is the solid, outer part of the Earth.
Informationen
- Beschreibung
- Constructive, destructive and conservative plate margins explained (GSCE)
- Erstellt von
- Becca Lyes · Mai 2015
- Aktualisiert
- 25 Apr 2016
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- 107
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