Structural data and samples were collected over a 70 km stretch from the Brandberg westwards up to the confluence of the Gemsbok River with the Ugab River. Fresh outcrops very near the coast have revealed a suite of cataclastic rocks that is of granitic origin and in which recrystallisation of low grade outlasted the cataclastic episode. The relationship of these rocks to the main rocks in the profile has yet to be determined.