The 600-cell lattice provides multiple geodesic routes between any two vertices. For a source CP and detector CP separated by \(L\) lattice steps, the number of geodesics scales combinatorially:
Coherence is maintained when phase differences between paths remain within the coherence window set by sea_strength: \(|\Delta\phi| < \pi \cdot \text{sea\_strength}^{-1}\). Decoherence occurs when bit-sea interactions introduce random phase shifts destroying path coherence.