Compressieveld — Aarde

Strata band density increases toward one edge — progressive geological compression. Ridge fractures appear where rock cracks under pressure. Warm sienna earth tones.

Horizontal strata form stacked, wavering bands across a tall frame. Sienna and gray lanes transition through soft gradients while deep black ridges cut crisp silhouettes that read as elevated contours. Fine pixel-level texture infills each band with granular chatter, increasing surface complexity without breaking the dominant layering. Subtle vertical undulation displaces the strata, creating recurring crests and shallow basins.