[en] La question ne s'est jamais posée de savoir comment l'Amblève (et l'Ourthe dans une prochaine note) a pu traverser les plateaux de Haute Belgique (et notamment le Massif de Stavelot-Venn), pour établir leur cours actuel. En présentant le bassin de l'Amblève et son histoire géologique, avec la première preuve sédimentaire de l'existence de l'amblève et en montrant l'influence de la structure géologique sur des tronçons de l'Amblève, les auteurs proposent leur réponse à cette question. [en] The question has never arisen of how the Amblève river (and the Ourthe in a future contribution) was able to cross the plateaus of Upper Belgium (and in particular the Stavelot-Venn Massif) to establish their current course. By presenting the Amblève basin and its geological history, with the first sedimentary proof of the existence of the Amblève and by showing the influence of the geological structure on sections of the Amblève, the authors propose their response to that question.
Disciplines :
Earth sciences & physical geography
Author, co-author :
Juvigné, Etienne ; Université de Liège - ULiège > Département de géographie
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