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Estructura interna de la tierra

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Estructura interna de la tierra

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About this activity

El planeta Tierra no es homogéneo, sino que está formado por capas concéntricas con diferentes materiales, espesores y propiedades:

Created by

José Daniel Miranda Alcoser
José Daniel Miranda Alcoser
Bolivia

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Estructura interna de la tierra
 

Estructura interna de la tierraOnline version

El planeta Tierra no es homogéneo, sino que está formado por capas concéntricas con diferentes materiales, espesores y propiedades:

by José Daniel Miranda Alcoser
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Explicación

Ejemplo local: La Cordillera de los Andes se formó por el choque de la placa de Nazca contra la Sudamericana.

El manto está compuesto por rocas ricas en hierro y magnesio, y es la zona donde se originan los movimientos de magma

El manto está compuesto por rocas ricas en hierro y magnesio, y es la zona donde se originan los movimientos de magma.

Se extiende entre 2.900 y 5.100 km de profundidad. Está formado por hierro y níquel en estado líquido.

Se encuentra en el centro de la Tierra, desde los 5.100 hasta los 6.371 km de profundidad. Compuesto principalmente por hierro y níquel en estado sólido debido a la enorme presión

 
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