Un curieux phénomène d'érosion famennienne: les "pains de grès" de Chambralles (Ardenne belge) ; A strange erosion phenomenon in Famennian stratas: the "wash-loaves" of Chambralles ( Belgian Ardenne)
peer reviewed ; Vertical walls in quarries of Famennian sandstones near Aywaille (Belgian Ardenne) show varied sedimentary structures. The most interesting are erosional effects on a few islets (or promontories) of a former sandstone layer that are bordered by micro-cliffs. Rounded and sub-circular "wash-loaves" accompanied by smaller and less regular masses occur near and outside of these cliffs. ; Les carrières de Chambralles, ouvertes dans les bancs de grès verticaux du Famennien supérieur, montrent une grande variété de structures péné-contemporaines de la sédimentation. On y note en parti... Mehr ...
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| Dokumenttyp: | journal article |
| Erscheinungsdatum: | 1965 |
| Verlag/Hrsg.: |
Elsevier
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| Schlagwörter: | sedimentology / Famennian / Belgium / sédimentologie / Famennien / Belgique / Physical / chemical / mathematical & earth Sciences / Earth sciences & physical geography / Physique / chimie / mathématiques & sciences de la terre / Sciences de la terre & géographie physique |
| Sprache: | Französisch |
| Permalink: | https://search.fid-benelux.de/Record/base-26513410 |
| Datenquelle: | BASE; Originalkatalog |
| Powered By: | BASE |
| Link(s) : | https://orbi.uliege.be/handle/2268/151142 |
peer reviewed ; Vertical walls in quarries of Famennian sandstones near Aywaille (Belgian Ardenne) show varied sedimentary structures. The most interesting are erosional effects on a few islets (or promontories) of a former sandstone layer that are bordered by micro-cliffs. Rounded and sub-circular "wash-loaves" accompanied by smaller and less regular masses occur near and outside of these cliffs. ; Les carrières de Chambralles, ouvertes dans les bancs de grès verticaux du Famennien supérieur, montrent une grande variété de structures péné-contemporaines de la sédimentation. On y note en particulier, sur un banc largement dégagé, des îlots souvent limités par des micro-falaises et de petites masses de grès isolées, de forme arrondie ("pains de grès").