Glacial Grooves Mesh Model

This post introduces the Glacial Grooves Mesh Model, a high‑resolution 3D reconstruction of the glacial grooves at Kelleys Island. Instead of treating grooves as static marks, the mesh functions as a spatial analytic instrument that reveals force directions, pressure regimes, and material interactions over deep time, making subglacial processes legible at human scale. The Substack article explains how this continuous surface enables comparison, measurement, and deeper reasoning about terrain shaped by ice and informs landscape interpretation without reducing it to simple diagrams or labels. For the full model details and conceptual framing, see the original post on Substack.