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relieve dos

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relieve dos

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relieve dis

Created by

Elisa Alonso Villa
Elisa Alonso Villa
Spain

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relieve dos
 

relieve dosOnline version

relieve dis

by Elisa Alonso Villa
1

Conjunto de formas muy peculiares características de las zonas de caliza, roca dura y rígida pero que se disuelve fácilmente con el agua de lluvia enriquecida con CO2. Ejemplo de estas formas son los lapiaces, dolinas, cuevas, cañones, simas, etc.

2

Es una extensión de tierra que está rodeada de agua por todas partes excepto por una zona o istmo que la une al continente.

3

Cauce fluvial seco que solo lleva agua esporádicamente, cuando descargan fuertes aguaceros, por lo que tienen un carácter torrencial. Son características de la vertiente mediterránea.

4

Las formas del relieve surgidas en el Terciario a consecuencia de la orogenia alpina. En la Península Ibérica se corresponde con los Pirineos, las Cordilleras Béticas, la Cordillera Costero-Catalana, el Sistema Ibérico, los Montes Vascos y la parte oriental de la Cordillera Cantábrica.

5

Las formas de relieve surgidas en la Era Primaria o Paleozoica a consecuencia de la orogénesis herciniana. Este relieve fue barrido durante la Era Secundaria y revitalizado por la orogénesis alpina en el Terciario.

6

Son entrantes costeros que resultan de la invasión por el mar del tramo final de un valle fluvial. Este hecho puede deberse al ascenso del nivel del mar o al descenso de la corteza continental

7

Llanura o meseta que se formó en la era primaria al erosionarse las cordilleras surgidas en la orogénesis herciniana. Forma la base de posteriores cuencas sedimentarias y cordilleras. En España ocupan extensas áreas en la mitad occidental de la península.

 
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