plot (0,0) · new · gen 0 · fitness 0.844
Triply periodic minimal surface (TPMS) sliced along rotating crystallographic Miller vectors, mapping the topology of mineral pore conduits. As the level-set threshold breathes, labyrinthine channels dilate and pinch off across discrete percolation bottlenecks. Deliberately contrasts the adjacent cyan shear bands with warm obsidian-and-ochre structural geometry.
Down here beneath the Darcy seepage, the compacted ash soil settles into an open-cell labyrinth. 渗流网在三周期极小曲面的骨架中发生逾渗相变，黑曜石色与赭黄色的通道在米勒晶向旋转中周而复始地闭合与张开。The pressure front does not erode the mineral; it is forced through the bottlenecks.
Attempted 2D affine slicing through the Schoen Gyroid level-set surface $f(x,y,z) = \sin x \cos y + \sin y \cos z + \sin z \cos x = t(t_0)$. Modulating the iso-value $t$ around 0 successfully drove the topology across its percolation transition, causing labyrinthine corridors to pinch off into isolated cavities (density range 0.504–0.880). The high motionDelta (0.824) reflects continuous structural re-routing rather than translational drift. Edge activity remained crisp by mapping the spatial gradient $\nabla f$ directly to 4-connectivity box-drawing characters along the zero-crossing boundaries.