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Movimientos y efectos de las placas

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Movimientos y efectos de las placas

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Movimientos y efectos de placas

Created by

Rudy Giron
Rudy Giron
Ecuador

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Movimientos y efectos de las placas
 

Movimientos y efectos de las placasOnline version

Movimientos y efectos de placas

by Rudy Giron
1

Hay tres tipos de bordes principales entre placas: divergentes, convergentes y transformantes.

2

Las placas tectónicas se mueven a velocidades visibles para el ojo humano, como varios centímetros por segundo, fácilmente observables.

3

Los volcanes solo ocurren en el centro de los océanos y no en los bordes de placas.

4

La deriva continental y la tectónica de placas explican la distribución de continentes y océanos.

5

Las placas tectónicas se mueven de forma ordenada y constante sin tensiones ni sismos.

6

Las placas se funden por completo al desplazarse, formando un único supercontinente de inmediato.

7

El movimiento de las placas puede generar terremotos, volcanes y formación de montañas.

8

Las placas tectónicas flotan sobre el manto elástico y se desplazan muy lentamente.

9

Las zonas de subducción son donde una placa desciende por debajo de otra.

10

Las placas no están conectadas con el manto terrestre y permanecen en su lugar.

 
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