Breuklijn — Cyaan Verschuiving

Diagonal shear splits horizontal strata bands. Ridge fractures cross the fault as cyan emerges. Five techniques, Floyd-Steinberg dithered for organic texture.

Undulating horizontal bands stack across the full field, alternating charcoal troughs with silver plateaus. Turquoise ridgelines trace each boundary, forming repeated wave contours that drift laterally as they descend. Fine granular texture and soft edge transitions create a misted gradient between strata while preserving crisp band separation.