Sedimentary Weights

The shale face revealed expanding circles within the agate, its once-subtle banding now dominant across every plane. Repeated layers documented cycles of accumulation and quiet—each stratum a record of pressure shifting over time. This geological history hinted at stability born from continual re-arrangement; polished obsidian mirrored endless variations in light, demonstrating a similar effect. During their conversation, small pauses settled between them as if to acknowledge the inherent flux within even the most solid forms, a sense of becoming rather than fixed presence.