
An experience where stark contrasts of light and shadow create shifting geometric planes that distort spatial perception, evoking a tactile sensation of space folding and unfolding. The interplay of c
**Abstract Visual Experiment Prompt — Divergent Image B (“Chasm / Vergence Stratified”)** ═══════════════════════════════════════════════════════════════════ **PRIMITIVE**: *The protagonist is a hyperbolic saddle — a negative Gaussian curvature surface, appearing as an expansive, undulating chasm, its anticlastic geometry repeated and accumulated in layered striations. Each “layer” or “band” is a cross-sectional slice of the hyperbolic surface, together constructing a geological profile of opposing depths converging toward the central band, yet never fully closing the gap. The “chasm” is a cut—an infinite recession—traversing horizontally across the image as a yawning negative space. Each band warps and buckles, accentuating the continuous negotiation between approach and recess, presence and void.* ═══════════════════════════════════════════════════════════════════ **COMPOSITION — HORIZONTAL GEOLOGICAL STRATIFICATION**: - The scene is organized into six to eight bold horizontal bands, each a layer of the chasm primitive, stacked with deliberate irregularity across the frame. - Bands are seen in section — edged, crisp, yet each inflected with saddle curvature (not flat strips). - Spatially, the deepest “cut” or negative gap is midway up the image, with upper bands arching downward into the chasm and lower bands arcing upward, visually squeezing emptiness between their razor inflections. - The emptiness of the central chasm — a thin, matte-black void — slices across the width in a slightly undulating horizontal course, never touching the edges of the frame, always held open by the warped “strata.” - Every band subtly shifts its hue and luminance along a left-to-right imperceptible gradient: a geological timeline in color. Only when the viewer compares the extreme left and right edges do they perceive the transformation from a cool mineral teal (left) to a deep volcanic umber (right). - No vertical dominance, no symmetry: the form unfolds horizontally — a cr