Step 1: Define the Mohorovičić Discontinuity (Moho). The Moho marks the boundary between the Earth's crust and mantle.
Step 2: Explain how it's found. The Moho is identified by a sudden increase in seismic wave speed (P-waves and S-waves). This speed increase happens because the mantle is denser and more solid than the crust.
Step 3: Detail the velocity change. P-wave velocity in the lower crust is usually 6.7–7.2 km/s. Crossing into the mantle, it jumps to 7.6–8.6 km/s. Thus, the Moho is characterized by a sharp P-wave velocity increase to over 7.6 km/s.
Conclusion: Option (B) best describes this seismic velocity change.