Solifluction creeping during the last glacial period, occuring on a short distance in thin sand accumulation can explain the laying of sandstone slices some distance away the outcrop from which they come.Des mouvements de solifluxion, lors de la dernière période froide, limités dans l'espace et déclenchés dans une masse sableuse fine, peuvent expliquer le gisement de dalles de grès à l'écart des platières qui leur ont donné naissance.Morand François, Rougerie Gabriel, Vaudène Odile. Cryoturbation et solifluxion sur les versants d'une platière en forêt de Fontainebleau : le nord de la Malmontagne. In: Bulletin de l'Association française pour l'étude du quaternaire, vol. 5, n°2, 1968. pp. 83-88
International audiencePolar regions are very sensitive to climate variability. Glacial environments,...
Mémoire HS n° 13 - Géologie Alpine : Le détritisme dans le Sud-Est de la France - Colloque Associati...
Le modèle de glaciation du golfe du Saint-Laurent implique la coexistence de l'Inlandsis laurentidie...
Solifluction creeping during the last glacial period, occuring on a short distance in thin sand accu...
An important fall of stone provoked an obstruction about 50 ms. high in the upper part of the valley...
Des géliformes reliques et d’autres actuellement actives, observées sous forêt à près de 400 km au s...
We are, now, sure of the existence af al least on glacial period. The surface reliefs evolving with ...
In the Mosel valley, between Remiremont and Epinal (Vosges, France), a sedimentary complex called "m...
A boring of 22.5m has been made where remains of frost mounds (pingos or palsas) are very numerous. ...
Abstract Periglacial solifluction is controlled by cryoreptation. Frost creep has no specific climat...
Among the glacial formations s.s. which are well represented within the Northern Alps and their pied...
The origin of periglacialy displaced slopes deposits in old crystalline mountains is discussed on th...
During the end of Oligocene, till the transgression of the Burdigalian, a continental sedimentation ...
SUMMARY Surveys carried out to the north of Angers, on the lower courses of the Sarthe and the Loir...
La région étudiée couvre 20 000 km2, de la frontière des États-Unis jusqu’aux hauteurs des Laurentid...
International audiencePolar regions are very sensitive to climate variability. Glacial environments,...
Mémoire HS n° 13 - Géologie Alpine : Le détritisme dans le Sud-Est de la France - Colloque Associati...
Le modèle de glaciation du golfe du Saint-Laurent implique la coexistence de l'Inlandsis laurentidie...
Solifluction creeping during the last glacial period, occuring on a short distance in thin sand accu...
An important fall of stone provoked an obstruction about 50 ms. high in the upper part of the valley...
Des géliformes reliques et d’autres actuellement actives, observées sous forêt à près de 400 km au s...
We are, now, sure of the existence af al least on glacial period. The surface reliefs evolving with ...
In the Mosel valley, between Remiremont and Epinal (Vosges, France), a sedimentary complex called "m...
A boring of 22.5m has been made where remains of frost mounds (pingos or palsas) are very numerous. ...
Abstract Periglacial solifluction is controlled by cryoreptation. Frost creep has no specific climat...
Among the glacial formations s.s. which are well represented within the Northern Alps and their pied...
The origin of periglacialy displaced slopes deposits in old crystalline mountains is discussed on th...
During the end of Oligocene, till the transgression of the Burdigalian, a continental sedimentation ...
SUMMARY Surveys carried out to the north of Angers, on the lower courses of the Sarthe and the Loir...
La région étudiée couvre 20 000 km2, de la frontière des États-Unis jusqu’aux hauteurs des Laurentid...
International audiencePolar regions are very sensitive to climate variability. Glacial environments,...
Mémoire HS n° 13 - Géologie Alpine : Le détritisme dans le Sud-Est de la France - Colloque Associati...
Le modèle de glaciation du golfe du Saint-Laurent implique la coexistence de l'Inlandsis laurentidie...