RUTA 2 PUNTO 11

 Punto 11. "Tapiología" la geología y su entorno (Plano Ruta 2)

Este muro se ha construido utilizando diferentes rocas de su entorno, podemos prácticamente indicar de forma clara, donde ha salido todas o casi todas las rocas que lo forman.

Si miramos en detalle vemos varias rocas con los ya clásicos rudistas, (estos tubos o agujeros circulares en las rocas).

Encontramos aquí rudistas de diverso origen y tipología, que nos permite hacer un repaso por la paleontología regional.

1) Hippurites incisus: caracterizado por su morfología irregular con dos tabiques muy marcados en la concha lo que genera dos grandes arrugas en el espacio interior.

2) Biradiolites canalictus: de diámetro más bien fino y largos, destacan por no tener esos pilares interiores, y sin embargo tienen una concha muy gruesa y redoblada.

3) Radiolites sauvagesi: de diámetro grueso sin pilares interiores, y concha muy gruesa con diferentes laminas que se superponen; lo que da una apariencia externa de "falda de gitana".




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ROUTE 1 WAYPOINT 8, ROUTE 2 WAYPOINT 4 AND ROUTE 3 WAYPOINT 4

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Plano ruta 1 (Científica)

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 La ruta 1 contempla 24 puntos de interés del 1 al 23 con el 8 y 8 bis. Enlace Ruta 1 en wikiloc con los 24 puntos y sus imágenes Descárgate la audio guía gratuita, en  Audioguidesapp,   para hacer el recorrido, y búscala en el mapa, o como creador, Arrecife de Castrojimeno. No te olvides de dar tu valoración al final del recorrido.
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ROUTE 1 WAYPOINT 12

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  Waypoint 12: The meeting point rock      Map route 1 As we move on, we continue with the unit of Dolomites of Montejo. Here wwe can see similarities with waypoint 3 but increased in magnitude. If we saw previously eroded ground and diluted by water, here the effect is larger, generating big, well-formed exokarstic structures. It is outstanding the rock just in front of us, the meeting point rock, symbol of Castrojimeno. Here two paths meet (right and left) and that continue in the path we have been following until this point. This structure called "Tor" has remained isolated, even though a few metres away we can find similar structure of smaller size. It represents an isolated block of the large dolomitic unit were we find ourselves. Another curious fact is that if we take notice of the position of the strata, they are slightly tilted, more than the rest, which determines that this is possibly a dumped block or partially rotated.
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