Abstract
This note describes evidence that thin diamicts which overlie the Galson Beach, previously interpreted as solifluction deposits are largely in situ glacial deposits. It is highly likely that all of north-west Lewis was covered by ice in the Late Devensian and that the maximum ice limit during this episode lay well to the west of the Hebridean Shelf. -from Author
Original language | English |
---|---|
Pages (from-to) | 1-7 |
Number of pages | 7 |
Journal | Quaternary Newsletter |
Volume | 76 |
Publication status | Published - 1995 |