Among the numerous problems of morphology in the Quebec section of the St. Lawrence valley, one of the most interesting and debatable problems is the late-glacial and postglacial chronology. The succession of other morphological events depends upon this chronology. How the inlandsis retreated ? When and under which climate ? Were there any glacial recurrences ? What has been the length of the postglacial erosion period ? Was there enough time for the normal erosion to shape the fluvial forms in the bedrock since the ice retreat or not ? These are some of the questions raised in this article
Les travaux présentés dans ce mémoire ont pour but de mieux définir et quantifier lesprocessus d’éro...
Glacial tongues, reaching down from the north by way of the valleys on both sides of Mont Tremblant,...
This is a systematic study of karsts in Eastern Canada especially caves and underground streams. The...
The morphology of the Québec region and the lower St. Lawrence valley is reappraised in this article...
Although major progress has been made in several research topics on the Laurentide Ice Sheet, there ...
The middle and upper Estuary regions of the St. Lawrence River include the Laurentian highlands to t...
River valleys in the Humber River drainage basin have derived most of their morphology from processe...
The erosive response to land surface deformation provides a record of isostatic variations and local...
A series of late Wisconsinan sedimentary sequences occupy parts of the Coppermine River valley, and ...
Les connaissances sur l’évolution morphoclimatique des Alpes pendant le Tardiglaciaire et l’Holocène...
The record of the Laurentide Ice Sheet is not well preserved in terrestrial deposits. Sediment seque...
The reconstruction of glacial chronologies during the Holocene (i.e. the past 11.7 ka) provides valu...
The study presented in this PhD memory aim at better define and quantify the present timeerosion pro...
Wholly submerged during the Mesozoic. the Drac basin area began to emerge by the end of the Cretaceo...
In the Great Lakes region, the vertical motion of crustal rebound since the last glaciation has dece...
Les travaux présentés dans ce mémoire ont pour but de mieux définir et quantifier lesprocessus d’éro...
Glacial tongues, reaching down from the north by way of the valleys on both sides of Mont Tremblant,...
This is a systematic study of karsts in Eastern Canada especially caves and underground streams. The...
The morphology of the Québec region and the lower St. Lawrence valley is reappraised in this article...
Although major progress has been made in several research topics on the Laurentide Ice Sheet, there ...
The middle and upper Estuary regions of the St. Lawrence River include the Laurentian highlands to t...
River valleys in the Humber River drainage basin have derived most of their morphology from processe...
The erosive response to land surface deformation provides a record of isostatic variations and local...
A series of late Wisconsinan sedimentary sequences occupy parts of the Coppermine River valley, and ...
Les connaissances sur l’évolution morphoclimatique des Alpes pendant le Tardiglaciaire et l’Holocène...
The record of the Laurentide Ice Sheet is not well preserved in terrestrial deposits. Sediment seque...
The reconstruction of glacial chronologies during the Holocene (i.e. the past 11.7 ka) provides valu...
The study presented in this PhD memory aim at better define and quantify the present timeerosion pro...
Wholly submerged during the Mesozoic. the Drac basin area began to emerge by the end of the Cretaceo...
In the Great Lakes region, the vertical motion of crustal rebound since the last glaciation has dece...
Les travaux présentés dans ce mémoire ont pour but de mieux définir et quantifier lesprocessus d’éro...
Glacial tongues, reaching down from the north by way of the valleys on both sides of Mont Tremblant,...
This is a systematic study of karsts in Eastern Canada especially caves and underground streams. The...