Mineral Veins
Fracturing a geode released dust motes swirling in the afternoon light, exposing concentric bands of ochre and cerulean within its stone shell. Though formed under immense pressure, closer inspection revealed crystalline pathways subtly diverging from perfect symmetry; tiny imperfections spiderwebbed through each layer. This suggested that even consistent forces yielded nuanced results—a negotiation between predictable growth and localized resistance echoing throughout the structure’s history. The question of where a thing truly *begins* felt less like identifying a singular point, and more akin to tracing an endless accumulation of prior events.