Reconstructions of past ice-flow provide useful insights into the long-term behaviour of past
ice sheets and help to understand how glaciated landscapes are shaped. Here, we present …

The erodent layer hypothesis (ELH) proposes that drumlinization leaves no substantial
stratigraphic record because it is primarily an erosional process that cuts an unconformity …

Little work has been completed on paleo-ice-sheet flow indicators of the Laurentide Ice
Sheet, west of the Keewatin Ice Divide. Field mapping, sampling and analysis of glaciogenic …

In combining and revising the two titles' Past Glacial Environments' and'Modern Glacial
Environments', Dr Menzies and his contributors provide the most comprehensive and wide …

Abstract At the Gibraltar porphyry Cu-Mo deposit in south-central British Columbia, Canada,
geochemical and mineralogical anomalies in till around a cluster of mineral occurrences …

Laurentide Ice Sheet (LIS) reconstructions beyond the last glacial maximum (LGM) are
difficult due to the incomplete stratigraphic record that has largely been eroded by the most …

The formation of drumlins remains a major enigma. It is accepted that drumlins form under
active temperate ice most likely within a soft sediment deforming bed at ephemeral 'sticky …

Deposits of the Vistula Ice Stream draining the Scandinavian Ice Sheet during the Last
Glaciation were investigated at four field sites in north-central Poland using micro-and …

The area of the Kashubian Coastland and areas adjacent to the northern part of the Lower
Vistula Valley (northern Poland) were involved in the major transgressive phases …

Abstract The Aberdeen Lake region of central mainland Nunavut is a former core region of
the Laurentide Ice Sheet that is characterized by streamlined glacial landforms classified …