RUTA 3 PUNTO 5

Punto 5. La canal de lavar y los bebederos (Plano Ruta 3)

Bajando al Arroyo de la Fuente del Prado o fuente Grande y tras haber pasado La Puentecilla y dejado a la izquierda Los Colmenares, se llega a la parte alta de La Canal, lugar donde se lavaba la ropa y cogía agua para la población cuando no estaba metida el agua en las viviendas.

Un poco más arriba había dos pilas de piedra, ( actualmente sirven de jardineras junto a la Asociación y en la plaza del Empedrado) donde bebían las caballerias cuando venían del campo de trabajar.


Llama la atención una roca con una estratificación cruzada muy marcada. La estratificación cruzada es una estructura interna debido al origen sedimentario de las rocas y que se relaciona con el movimiento de corrientes (normalmente agua) y que genera estructuras llamadas Ripples o dunas submarinas que van moviéndose gracias a las corrientes.



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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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