Calcite formations swell

Calcite formations swell within the cave, their growth charted in meticulous notes despite an absence of predictable rhythm. Layer upon layer builds not through seamless addition, but from countless minute interruptions—air bubbles trapped mid-flow, grains of sediment shifting with the damp air. The stone’s cool smoothness belies a continuous yielding to pressure; each stratum demonstrates how even apparent solidity is woven from resistance and response. Heat radiating from deeper earth subtly alters these patterns over millennia, leaving records etched in crystalline structure that don't easily reveal their origin—a quiet weight accumulating time.