Prismatische Breuk — Gesplitst

Tectonic fault rendered then split into R/G/B channels by chromatic aberration. Colors separate at the fault line like light through a prism. The geological becomes the optical.

Jagged vertical slabs in dark slate gray dominate a tall frame, establishing repeated rift-like columns. Cyan islands and maroon shards interleave between slabs, forming hard-edged breaks and cutout silhouettes. Fine speckled texture and grainy fill add micro-variation inside larger flat shapes. Overlapping bands create layered depth through occlusion and abrupt color transitions.