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Metamorphose und Magmatismus in Venn-Stavelot-Massiv, Ardenen. (Metamorphosis and magmatism in the Venn-Stavelot-Massif, Ardennes)
Ardenne ; Belgique ; Cristallin ; Géographie de l'Europe ; Plissement ; Pétrogenèse ; Socle ; Tectonique ; Venn-Stavelot, massif
The Venn-Stavelot Massif is the eastermost of four upfolded massifs which make outcropping the pre-Variscan basement of northwestern Europe. The Venn-Stavelot Massif has a huge petrological, historical-geological and geodynamical importance, which

Hercynische invloed op Noord-en Zuidrand van het Massief van Stavelot. Probleem der N-S plooien. (Hercynian influence of the north and south edge of the Stavelot Massif. N-S foldings problem)
Belgique ; Flexure ; Géographie de l'Europe ; Hercynien ; Socle ; Stavelot massif ; Tectonique

The Stavelot Massif from Cambrian to recent. A survey of the present state of knowledge
At the occasion of the annual Meuse-Rhine geologists meeting at Mont Rigi (Hautes Fagnes, Stavelot Massif) on May 18-19, 1990, a review has been prepared on the geology of the Stavelot Massif. It illustrates the actual state of the art, achievements

Acid igneous rocks of Stavelot Massif, a case of Pre-Hercynian weathering
Belgique ; Cristallin ; Géographie de l'Europe ; Liège ; Météorisation pré-hercynienne ; Pétrologie ; Stavelot, massif
Acid intrusive and extrusive rocks of the Stavelot Massif (Belgium) have been analyzed for major-and trace elements. The extrusive rocks have been subjected to pre-or syndiagenetic weathering, during which process biotite was a stable mineral

Découverte d'une discordance angulaire dans le socle anté-varisque du massif de Stavelot (Ardenne)
Belgique ; Cambrien ; Discordance angulaire ; Ere primaire ; Géographie de l'Europe ; Géologie régionale ; Liège, prov. ; Stavelot, massif ; Tectonique
In the Stavelot Massif an angular unconformity has been found within the Devillian, the highest part of which is of early Cambrian age. This unconformity is either intra-Cambrian or just at the base of the Cambrian succession. (Les AA).

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

Télédétection appliquée dans le Massif de Stavelot (Belgique) in Musée royal de l'Afrique Centrale. Rapport annuel 1987-1988. Département Géologie et Minéralogie.
Belgique ; Géographie de l'Europe ; Géologie régionale ; Landsat ; Linéament ; Sructure géologique ; Stavelot Massif ; Thematic Mapper ; Télédétection

Aachen, région ; Allemagne de l'Ouest ; Ardennes, massif ; Belgique ; Guide touristique ; Géographie de l'Europe ; Hautes Fagnes ; Hohe Venn ; Limburg ; Nordrhein-Westfalen ; Pays-Bas ; Paysage ; Tourisme
Huit commentaires précis et pédagogiques des paysages de la région d'Aix-la-Chapelle: le centre, le bassin charbonnier, le piémont de la Venn, la haute Venn, le bassin calcaire de Prüm, Aix, Lüttich-Maastricht: centres urbains du triangle frontalier

The purpose of this paper is to estimate the influence of the land use and the water balance on the dissolved load budget in drainage basins on silicate rocks. The water balance in the Hohes Venn and the Rureifel areas is mainly influenced
by decreasing rainfall intensity from the Hohes Venn towards NE. Furthermore, different organic and anorganic soil properties influence the water balance in these areas. The investigation of stream load indicates regional differences of water chemistry

Many observations collected along the E42 highway, between Born (Massif de Stavelot) and the Our valley (south of Sankt-Vith) give a detailed portrait of the Eodevonian lithological succession in this part of the Eifel Synclinorium. Six structural

A Permian conglomerate of continental origin, the Malmédy Puddingstone, extends across the Cambrian massif of Stavelot. The conglomerate has three successive units, the middle one comprising predominantly limestone pebbles in a calcareous

. The AA. demonstrate here that lithalsas were formed only on weathered quartzitic rocks of the Cambro-Ordovician massif of Stavelot, and probably are associated with local hydrological conditions.

Distribution and ecology of H. armoricum are studied in the Ardennes massif. Known from 24 IFB-squares (16km) before 1930, it is recorded today from 59 IFB-squares: 38 from the Stavelot Cambro-Ordovician massif, 18 from the Rocroi massif and 3

Une étude de la répartition de mégalithes dans la vallée de l’Amblève à sa traversée des quartzites d’âge cambrien de la formation de la Venne à l‘extrémité occidentale de la crête de la Vecquée a été réalisée. Elle a permis de montrer que les

Monographie de Grevenbroich (28000h) sur la moyenne terrasse de la rive gauche du Rhin, de Eschweiler (39000h) et Würselen (20000h) au pied de l'Eifel et de la Venn. Würselen et Eschweiler ont développé une métallurgie précoce (fer de l'Eifel, bois

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