Plano ruta 2 (Urbana)

La ruta comienza en las Escuelas y 2 consta de 15 puntos  el 4-5-9 y 10 son compartidos con la ruta 1 y recorre las calles de Castrojimeno y se puede hacer en una 1 hora.

Enlace Ruta 2 en Wikiloc con sus 15 puntos y fotografias

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 3 WAYPOINT 5

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Waypoint 5. The washing channel and the drinking troughs   (Route Map 3) Going down to the Arroyo de la Fuente del Prado or Fuente Grande and after passing La Puentecilla and leaving Los Colmenares on the left, you reach the upper part of La Canal, a place where people washed their clothes and fetched water for the population when the water was not piped into the houses. A little further up there were two stone basins (currently used as planters next to the Association and in the Plaza del Empedrado) where the horses drank when they came from the fields to work. A rock with a very marked cross stratification is striking. Cross stratification is an internal structure due to the sedimentary origin of the rocks and is related to the movement of currents (usually water) and generates structures called Ripples or submarine dunes that are moving thanks to the currents.
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ROUTE 1 WAYPOINT 6 AND ROUTE 3 WAYPOINT 2

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  Waypoint 6: First meters of the stratigraphic bar  (Map route 1)   (Map route 3) As we take the "La Muela" street and follow our journey to the "Sancta Santorum" we cannot underestimate what we have been watching before, and what we will see now. The eastward orientation of the rock and the local climate has provoqued that this waypoint is especially covered with lichens, moss and grassy plants. It is for this reason that we have to closely listen to this waypoint, focusing on the bibliography, it stands out an article from 2009 published about Facies. Here we find the Facies A, a chalky rock dominated with calcius "mud" with fragment of fossils. Lets outline the presence of "Orbitolinas" a genre of foraminiferal species that lived in the Cretaceous seas, the foraminiferal species, as are microscopic organisms they are not visible to the naked eye. These rocks are associated to stormy episodes and times of stability that generate this successio
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RUTA 1 PUNTO 11

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Punto 11: Vista panorámica Peñas del Cuervo  (Plano Ruta 1) Avanzamos y ahora miramos hacia el reguero de La Hoz.  Los desprendimientos son algo común, y natural que se debe a la erosión continua en los que en ciertos momentos se pierda la estabilidad de la pared, favorecido por la congelación del agua de las grietas, en los duros inviernos, y se produzcan esos desprendimientos. En concreto lo que vemos aquí, es el desprendimiento de una gran roca sobre una tenada. Dice la tradición, que cayó cuando una pastora estaba guardando las ovejas y hoy en día sigue sepultada bajo esa gran mole de piedra.
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