Mapa mental
Restless Earth
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Restless Earth
Structure of the Earth
- Crust; outer layer, up to 75km thick
- Split into 2 types of crust; oceanic crust and continental crust
- Continental crust
- Granite
- Less dense
- Light
- Thin
- Old
- Oceanic crust
- Basalt
- Dense
- Heavy
- Thick
- New
- Continental crust
- Split into 2 types of crust; oceanic crust and continental crust
- Mantle (magma); up to 2800km thick
- The upper part forms part of the lithosphere and is rigid
- The lower part is semi-molten and forms part of the asthenosphere
- 1200 degrees celsius
- Outer core
- Has liquid properties
- 3000 degrees celsius
- Inner core
- Inner most part of the Earth
- 5000 degrees celsius
- Iron and nickel
- Crust; outer layer, up to 75km thick
Plate boundaries
- Destructive (colliding)
- Eurasian and Pacific
- Constructive (pull apart)
- Indo Australian and Antarctic
- Collision (two continents collide)
- Eurasian and Indo Australian; forming Himalayas
- Conservative (slide past)
- Pacific and North American
- East African Rift Valley
- A rising convection current (plume) creates a hot spot below the continental crust & weakens it, the diverging current splits the plates apart
- Continent splits, land sinks to from a rift valley with active volcanoes throughout the length
- Rift valley can collect water and form giant lakes
- Continent splits, land sinks to from a rift valley with active volcanoes throughout the length
- A rising convection current (plume) creates a hot spot below the continental crust & weakens it, the diverging current splits the plates apart
- Destructive (colliding)
Informações
- Descrição
- GCSE Geography Mapa Mental sobre Restless Earth, criado por Tamzin Elliott em 15-10-2016.
- Criado por
- Tamzin Elliott
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