The soil is composed of a layer of loess arable soil, with marl underneath (formations of Maastricht and Gulpen) and local occurrences of pleistocene and tertiary formations, such as old Maas gravel and the formations of Rupel, Tongeren, Holset and Hoogcruts.
Esos tres que acaban de salir han dejado claro...... lo que piensan de mí, el hijo tonto de Kyneeurlex-diff-2018-06-20 eurlex-diff-2018-06-20