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TEMA 5 LA GEOSFERA 2

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Capas y discontinuidades de la Tierra.

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TEMA 5 LA GEOSFERA 2
 

TEMA 5 LA GEOSFERA 2Online version

Capas y discontinuidades de la Tierra.

by PABLO MORENO JIMENEZ
1

La corteza continental está formada principalmente por basalto.

2

La discontinuidad de Gutenberg se sitúa a unos 2.900 km de profundidad.

3

El núcleo externo es sólido.

4

La discontinuidad de Weichert-Lehmann separa el manto externo del manto interno.

5

La corteza oceánica es más joven y delgada y está formada por basalto y gabro, con densidad media de 3 g/cm3.

6

El manto inferior tiene mayor densidad (5,5 g/cm3) que el manto superior.

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