These rocks have a complicated history. Some were sandstones, a sedimentary rock that forms as grains wash, tumble and settle while others were originally basalt, a rock formed from volcanoes. Both have been heated and altered, in some cases the heat has been so intense that the original rock has melted completely forming granite like textures.
Now, walking across these, exposed, rounded, bodies of rock, you will find evidence of this re-working. Across one rock face are the ripples of heat and pressure, minerals gathered and puckered into ribbons of tight folds. In a few places, mylonite fabrics run in delicate linearity marking moments of dynamic recrystallisation.