Answer:
True
Step-by-step explanation:
The D layer is a transition zone between the solid portion of the lower mantle and the liquid outer core. Because S-waves only travel through solids, it has been hypothesized that a partially molten transition zone would affect the velocity of these S-waves by slowing them down considerably as the rock layer becomes less solid. The waves that are able to travel through a non-solid medium are the P-waves, which are more energetic than S-waves.