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Cehegín nevado, Murcia
 murcia  2009/7/17 16:20
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| The municipal term of Cehegín concerns to the relief it divides in several areas. The south of the term, remains characterized for the mountainous upgrade gradients they occupy the majority of your surface and stops among them tight valleys.The central region and west, whose morphology is stood out for the presence of the Argus and Quípar rivers, with your wide valleys and extensive areas of terrace in a flat way and soft tilts.An area eastwards, characterized for mountainous upgrade gradients of smaller magnitude that the |mesozóicas| saws of the south form a very rural and discontinuous relief.The mountainous upgrade gradients align in the structural address SW-NE. this orientation is general in all of Bética.Normally, the more abrupt areas, with the more angle shapes and cut, give it limestones and dolomites. In contraposition, the marls and detrital rocks give more soft concave-convex leavings. Between both extremes, they exist all intermediate morphologies.[url=http://commons.wikimedia.org/wiki/File:127_2792.JPGFrancisco[/url] |
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Fotografias Pueblos de España
Region de Murcia
