← Iris

Spin ωz  0.00 rad/s
Pitch    0.00 rad/s
Roll     0.00 rad/s
Reversals 0
Live
Initial Spin Speed 8 rad/s
Chirality Offset 15 deg
Damping 0.008
Aspect Ratio a/b 2.5

Click canvas to give a random perturbation. Spin CW to see the instability; CCW to see stable spin.

How the Rattleback Works

A rattleback is a solid of revolution that is not symmetric about its vertical axis of spin. The principal axes of inertia are skewed relative to the geometric axes of the shell. This small angular offset — the chirality angle α — is enough to couple the three modes of oscillation: spin (ωz), pitch (ωx), and roll (ωy).

When you spin the rattleback in its unstable direction, small perturbations excite pitching oscillations. The pitch mode is coupled back to the spin mode with the opposite sign — energy is extracted from the spin and pumped into pitch, then eventually returned as spin in the opposite direction. The mechanism is entirely Newtonian; there is no friction paradox or violation of conservation laws.

  • Stable direction: spin energy is not efficiently coupled to pitch; the stone spins freely until damped.
  • Unstable direction: coupling is strong; one full reversal cycle can take under a second at high chirality.
  • Multiple reversals: if energy loss is low enough, the stone can reverse 2–3 times before coming to rest.
  • Historical note: Celtic stone artifacts found in British museums show this effect; Walker described it in Scientific American (1979).

The Equations

The dynamics follow Euler's equations for rigid-body rotation on a curved surface. Let the rattleback have principal moments I₁, I₂, I₃ with inertia axes rotated by angle α from the geometric axes. The no-slip contact constraint on a flat surface adds reaction forces. The coupling terms proportional to sin(2α) drive the spin reversal — at α = 0 or 90° there is no coupling and no reversal.