with the Moine Thrust itself. It is thought to be the youngest formed thrust structure in the belt, which is consistent with a foreland propagating thrust sequence. Along strike the footwall of the Sole Thrust changes from Lewisian in the south to Cambrian in the north. Arnaboll Thrust In the Eriboll section this thrust carries Lewisian gneiss over the Pipe Rock. Its outcrop is complicated by the effects of later thrusting that both folds and offsets the Arnaboll Thrust. The exposures on the flank of Ben Arnaboll have particular importance as it was here that Lapworth first described the highly deformed rock type mylonite and also where Geikie coined the term "thrust plane". Ben More Thrust The Ben More Thrust is the largest and most continuous of the thrust faults developed between the Moine and Sole Thrusts within the Assynt Window. Glencoul Thrust This thrust is developed within the lower part of the belt in the Assynt Window. Kinlochewe Thrust The Kinlochewe Thrust branches off the Moine Thrust's central section and runs southwards past Kinlochewe to the Achnashellach Culmination, where it is truncated by the SW–NE trending Strathcarron Fault. It may originally have been continuous with the Kishorn Thrust. Kishorn Thrust The Kishorn Thrust extends from the Achnashellach Culmination, just north of Loch Carron, where it is truncated by the Strathcarron Fault. It continues southwestwards to Loch Kishorn, becoming the basal thrust. On the Isle of Skye, the Kishorn Thrust also marks the base of the Moine Thrust Belt bringing mainly Torridonian sandstones over foreland Cambrian-Ordovician limestones and quartzites. Locally on the Sleat peninsula the Kishorn thrust sheet is eroded to form the Ord window in which the foreland rocks once more appear. Tarskavaig Thrust At the southwestern end of the Sleat peninsula, the Tarskavaig Thrust carries Moine Supergroup metasediments over the Torridonian of the underlying Kishorn thrust sheet. Northward continuation When the MOIST (Moine and Outer Isles Seismic Traverse) deep seismic profile was acquired north of the Scottish mainland by the BIRPS group in 1981 a series of east-dipping fault zones were imaged, two of which were interpreted as potential continuations of the Moine Thrust. The presence of half graben basin in the hanging walls of these faults was interpreted to represent Devonian and Mesozoic extensional reactivation of the Caledonian thrust structures. Further deep profiles acquired in the same area, the DRUM and GRID lines confirmed these features. Onshore