Route 1

  - MAP ROUTE 1- 

01.- ROUTE 1 WAYPOINT 1          The initial loam soils   

02.- ROUTE 1 WAYPOINT 2          Start of the first bar

03.- ROUTE 1 WAYPOINT 3          External karstic processes

04.- ROUTE 1 WAYPOINT 4          Panoramic view of the stratigraphic succession

05.- ROUTE 1 WAYPOINT 5          The start of the second bar

06.- ROUTE 1 WAYPOINT 6          First meters of the stratigraphic bar

07.- ROUTE 1 WAYPOINT 7         The uso of chalky rocks in the village's

08.- ROUTE 1 WAYPOINT 8         The reef.

09.- ROUTE 1 WAYPOINT 8 BIS  Decorative blocks with rudists

10.- ROUTE 1 WAYPOINT 9         The Dolomites

11.- ROUTE 1 WAYPOINT 10       The Radiolites

12.- ROUTE 1 WAYPOINT 11       Panoramic view.

13.- ROUTE 1 WAYPOINT 12      The meeting point rock

14.- ROUTE 1 WAYPOINT 13      The sickles' cannon

15.- ROUTE 1 WAYPOINT 14      A cave thanks to a fault

16.- ROUTE 1 WAYPOINT 15      The chalky rock stairs

17.- ROUTE 1 WAYPOINT 16      Panoramic view

18.- ROUTE 1 WAYPOINT 17      The upper area

19.- ROUTE 1 WAYPOINT 18      Viewpoint of the antenna

20.- ROUTE 1 WAYPOINT 19     Oakum fields.

21.- ROUTE 1 WAYPOINT 20     The winepress

22.- ROUTE 1 WAYPOINT 21     The sinuous stairs

23.- ROUTE 1 WAYPOINT 22     The wineries path

24.- ROUTE 1 WAYPOINT 23     Quarry with crossed layering


Answer you need know in  https://poe.com/ArrecifeCastrojimeno


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ROUTE 3 WAYPOINT 5

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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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