13. Assilinas, discocyclinas and other at Salarons




    This is a site distributed across several strata that you cross as you come to the entrance of the Faja de las Flores natural terrace and path, with stratum surfaces containing considerable concentrations of foraminiferans. Geological unit T1.


    This is probably the site with the greatest concentration of these foraminiferans in Ordesa Park.


    After you have gone beyond the Carriata or Salarons pitons and the meadows that come after them, you go over a group of bare rocks and come to the entrance to the small Salarons Valley.
    The Faja de las Flores path turns eastward past various strata described as the site.

    A significant layer is to be found at the UTM coordinates 31T 256689 4726828.