Mica Basal Cleavage — Interlayer Peeling (2D)
A 2D cross-section of a mica crystal: weak interlayer bonds hold TOT sheets together while strong Si-O bonds fuse each sheet internally. Drive a wedge into an interlayer gap and peel sheets down to nanometer thinness, or try cutting across a sheet to see why that fails.
A cross-section of a mica crystal shows why the mineral has perfect basal cleavage: weak interlayer bonds let a wedge split off paper-thin sheets one at a time, while the strong covalent network inside each sheet resists cutting across it almost entirely.
A 2D companion to the 3D mica sorter, showing why mica splits at all: a cross-section of stacked TOT sheets held together only by weak interlayer bonds (K+ ions, van der Waals forces) between silicate layers that are themselves fused by strong covalent Si-O bonds. Drive a wedge into a chosen interlayer gap and push the splitting force past the cleavage threshold to peel off sheets down to nanometer thinness — then try forcing a crack straight through a sheet instead and watch it shatter rather than cleave, since in-plane bonding is roughly fifty to eighty times stronger.
2D · HTML5 Canvas 2D · 60 FPS target · runs fully client-side, no install