The Earth's crust plays a significant role in influencing the propagation of seismic waves. The different composition and density of materials in the Earth's crust cause seismic waves to change speed and direction as they travel through it. This can result in the reflection, refraction, and absorption of seismic waves, affecting their intensity and distribution. Additionally, the presence of fault lines and various geological structures in the crust can further impact the movement and behavior of seismic waves.