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2505604
Plate Tectonics
Descrição
Restless earth at Year 9 level
Sem etiquetas
gcse
Mapa Mental por
Anna Hadley
, atualizado more than 1 year ago
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Criado por
Anna Hadley
mais de 9 anos atrás
18
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Resumo de Recurso
Plate Tectonics
Volcanoes
Composite
Infrequent Erruptions but violent
Thick, sticky Larva
Shield
Frequent Erruptions
Thin Runny Larva
Inside the earth
In the mantle there is a convection current where the hot air rises and sinks when it cools
The crust is split into 14 major plates and 38 minor plates
Key Terms
Crust
Outer layer of the earth
Plate
A section of the earth's crust
Plate Margin
The boundary where 2 plates meet
Mantle
The dense layer
Semi-liquid layer
Convection currents
The process of air rising and sinking
Crust
Oceanic Crust
Newer- generally less than 200 million years old
Can possibly sink
Denser
Can be renewed and destroyed
Continental Crust
Can't sink
Older - More than 1500 million years old
Less dense
Cannot be destroyed or renewed
Plate Margins
Destructive Plate Margins
Where the plates move towards each other and collide
The most destructive is when a continental plate collides with a oceanic plate, the oceanic plate sinks bellow the continental. (subduction Zone)
Constructive
Where the plates move apart or diverge
A volcano is formed in the gap
COnservative Boundaries
Plates moving across each other
The plates are moving at different speeds in different directions
Anexos de mídia
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