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Placas tectónicas: completar conceptos

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Placas tectónicas: completar conceptos

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Completa conceptos sobre placas

Created by

MARTA LILIANA PAIZ DE ARGUETA
MARTA LILIANA PAIZ DE ARGUETA
El Salvador

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Placas tectónicas: completar conceptosOnline version

Completa conceptos sobre placas

by MARTA LILIANA PAIZ DE ARGUETA
1

Las son grandes bloques de la y el manto superior que se mueven muy poco al día , pero con el tiempo pueden desplazarse miles de kilómetros . Su movimiento da origen a diferentes límites : cuando estas placas chocan , se forman cadenas montañosas ; cuando se separan , hay expansión en la litosfera ; en los bordes donde una placa se desliza bajo otra se crean fosis oceánicas y actividad volcánica . Estas interacciones provocan sismos y cambios en el relieve , y explican la idea de la .

 
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