Current-bedding in the Moine series of northwestern Scotland

"This note records a number of observations of orientation of current-bedding in the Moine series of Inverness-shire, Wester Ross and Sutherland, in the north-western Highlands of Scotland. The foreset beds have been found to have a dominant dip towards the north, thus suggesting that the currents responsible for the transport of the material forming these beds flowed from the south."