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Along the eastern margin of the nappe folds verge to the east and the cleavage fans until it dips westward.
Moine rocks within the Moine nappe are mainly unmigmatized psammites which locally may preserve sedimentary structures.
Stratigraphic relationships show that the Mata nappe follows a recumbent fold structure characterized by a normal and an inverted fold limb.
Southwest of the Dornoch Firth, the Sgurr Beag Thrust divides the Moine rocks into two major nappes .
Another important difference is that the basement of one of the Menderes nappes (dine nappe, see below) is of Neoproterozoic to Cambrian age.
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