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Geometry of deformation adjacent to the Glencoul thrust at Loch Glencoul, Sutherland

Synopsis The Glencoul thrust at Loch Glencoul is on a ramp zone to which footwall imbricate faults are related. Lewisian rocks in the hanging wall are deformed against this ramp; dykes and the country rock foliation have been rotated into near-parallelism with the thrust plane. The degree of the deformation in the Lewisian gneiss and the dykes increases gradually towards the ramp surface.