Abstract
"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."
GeoRef, Copyright 2004, American Geological Institute. Reference includes data from Bibliography and Index of Geology Exclusive of North America, Geological Society of America, Boulder, CO, United States