File:Garganta y puente de El Villar.jpg
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Español: La garganta que forma el río Lozoya en este entorno, destaca como elemento geomorfológico de carácter erosivo, asociado a fenómenos fluviales. Corresponde a formas de incisión lineal, estrechas, cuyo desarrollo vertical (encajamiento) es mayor que su anchura, pudiendo tener condicionantes tectónicos. |
| Source | Own work |
| Author | Diego Sanz Siguero |
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I, the copyright holder of this work, release this work into the public domain. This applies worldwide. In some countries this may not be legally possible; if so: I grant anyone the right to use this work for any purpose, without any conditions, unless such conditions are required by law. |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 17:49, 7 June 2009 | | 1,024 × 768 (495 KB) | Dexter182 (talk | contribs) | {{Information |Description={{es|1=La garganta que forma el río Lozoya en este entorno, destaca como elemento geomorfológico de carácter erosivo, asociado a fenómenos fluviales. Corresponde a formas de incisión lineal, estrechas, cuyo desarrollo verti |
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