In the las few years the integral restoration of gravel extration land in alluvial soils has taken a very important role. The restoration proposal implies frequently a transformation to a wetland landscape (scenery), in which coexists restored zones above the phreatic level and residual lagoons. The borders of these lagoons must have a suitable lie and slop in order to allow the development of a wetland biotope.
Obviusly this restoration model suggests a change of use of the affected soi
