An outline of the geological structure of the Northeastern Hohes Venn Area and of its Northern foreland
Lower Paleozoic (Cambrian, Ordovician), Devonian, and Carboniferous sedimentary rocks are exposed in the northeastern part of the Hohes Venn area (Northern Eifel) and in its northern forelands. The regional geological development represented
by these sediments and their Caledonian and Variscan structural characteristics are obtained from geological profiles across the Eifel's northern boundary zone.