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Deriva continental y placas tectónicas

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Deriva continental y placas tectónicas

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Movimiento de continentes y placas

Created by

Adalgisa Ayala Guerrero
Adalgisa Ayala Guerrero
Dominican Republic

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Deriva continental y placas tectónicas
 

Deriva continental y placas tectónicasOnline version

Movimiento de continentes y placas

by Adalgisa Ayala Guerrero
1

Introducción a la deriva continental

La deriva continental propone que los continentes estuvieron unidos en el pasado y se separaron con el tiempo, formando las masas terrestres actuales.

2

Pruebas fósiles

Fósiles de especies similares en continentes opuestos, como dinosaurios y plantas, sugieren una antigua conexión entre África, Sudamérica y otras regiones.

3

Coincidencia de costas

Las costras costales encajan como piezas de rompecabezas, apoyando que los continentes estuvieron unidos previamente y se desplazaron a sus posiciones actuales.

4

Evidencias geológicas

Formaciones rocosas y cadenas montañosas continúan señales compatibles, como si hubieran formado un único cinturón tectónico en el pasado.

5

Placas tectónicas

Placas tectónicas son bloques grandes de litosfera que se mueven lentamente sobre el manto, interactuando en sus bordes.

6

Límites de placas: divergentes

En los límites divergentes, las placas se separan; se crean nuevas cortezas oceánicas mediante el ascenso de magma.

7

Límites de placas: convergentes

En límites convergentes, las placas chocan; se forman montañas o zonas de subducción, donde una placa se hunde bajo otra.

8

Límites de placas: transformantes

En límites transformantes, las placas deslizan lateralmente, provocando fallas y, a veces, sismos significativos.

9

Mecanismo de movimiento

La convección del manto empuja y guía el movimiento de las placas, dando origen a terremotos y volcanes.

10

Consecuencias y evidencia actual

Mediante GPS y satélites, observamos el desplazamiento continuo de placas; la teoría de la deriva abrió la comprensión de la geología moderna.
 
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