It splits along stress, not its own layers
Slate begins as mud, pressed and gently cooked into rock. Under the squeeze of mountain-building, its microscopic mica flakes all swing around to line up at right angles to the pressure, and the stone splits cleanly along that new grain. The strange part: this cleavage usually cuts across the original mud layers — so slate breaks the way the Earth squeezed it, not the way it was first laid down.