The slope where fallen rock comes to rest, down to about the wall’s own height below its foot, used to be grass and soil like the hillside. It is now gray broken rock. Open granite also carries lichen patches a few meters to fifteen across, so a slab 100 to 300 m away looks mottled, and the big talus boulders show pale granite scanned from real rock instead of a furry generated pattern.
Where a ledge meets a cliff, the ground and rock textures no longer stretch into streaks.
