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La subduction
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La divergence
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Les plaques tectoniq

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La subduction Quand une plaque océanique heurte une plaque continentale. Une plaque tectonique plonge sous l’autre.
La divergence c’est quand deux plaques océanique s'écartent. Le magma peut engouffrée la fissure sous l’eau.
La collision Quand deux plaques continentales entrent en collision. Ceci peut cause des montagnes.
La friction Quand deux plaques coulissent l’une contre l’autre et produit une grande friction- des tremblement de terre
les plaques tectoniques Morceaux plus ou moins grands de la lithosphère terrestre 53-7 grands -les continentset 46 petites-composé de croute terrestre et manteau
la lithosphère Couche externe de la croûte terrestre constituée de plaques mobiles.
Magma roche en fusion qui se forme à haute température (jusqu'à 1.200°
une couche 3- le noyau, le manteau et la croûte.
la croûte Zone superficielle du globe terrestre, d'une épaisseur moyenne de 30 km sous les continents, atteignant 70 km sous les chaînes de montagnes
Created by: Grozova Veronica
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