Shear structures in the Kohistan arc

Subsidiary shears which deform foliation within the Kohistan Arc.
Subsidiary shears which deform foliation within the Kohistan arc. These may be used to deduce the sense of shear along the early ductile contact between Kohistan and Nanga Parbat rocks.  Looking west across the Indus river. The visible cliff height is about 15m. Compare with the shear sense deduced from the shear band structure.