Final answer:
An earthquake transfers mechanical energy to the ocean, creating a tsunami with larger amplitude waves as they approach shallower coastal waters.
Step-by-step explanation:
An earthquake can generate a tsunami by causing a large displacement of the seafloor, which transfers a significant amount of energy to the ocean water above it. This energy transfer results in a series of waves with long wavelengths. The model described indicates that the amplitude of these waves is related to the energy imparted by the earthquake's seismic activity. As the waves travel into shallower coastal waters, their speed decreases, the waves compress, and the amplitude increases, making the tsunamis more visible and powerful as they approach the shore.
A correct answer to the model provided would be: An earthquake's seismic wave provides mechanical energy to the ocean. As energy is added, the amplitude of the wave is increased (Option A). This is because the amount of energy in a wave is directly proportional to its amplitude squared, which leads to larger ground displacements and the potential for significant coastal damage when these waves reach the shore.