It erodes them to be a different size and shape.
Seismic waves.
Waves slow down as they approach a shoreline. The first parts of the shoreline that waves meet are the headlands, or pieces of land that project into the water. The slowing waves bend toward the headlands, which concentrates the waves' energy. A huge amount of energy is released when waves crash into headlands, causing the land to erode.
The point where rocks break and release energy in the form of seismic waves is known as the focus or hypocenter of an earthquake. This is typically located beneath the Earth's surface along a fault line where the stress within the rocks exceeds their strength, causing them to fracture and generate seismic waves.
Waves are not created by rocks, but rather by the energy of wind moving over the surface of the water. Rocks on the ocean floor can influence the shape and direction of waves as they break and change the wave patterns.
It would generally take more wave energy to deposit rocks compared to sand. Rocks are typically heavier and more resistant to erosion, requiring stronger waves to move and deposit them. Sand, on the other hand, is lighter and easily transported by waves, making it less energy-intensive to deposit.
Crashing waves can cause erosion because the force and energy of the waves can wear down coastal rocks and cliffs over time. The constant impact of the waves can break apart rocks and carry away sediments, leading to the gradual erosion of the coastline.
The vibrations that occur when rocks break are called seismic waves. These waves are generated by the sudden release of energy during rock fractures and can travel through the Earth, causing earthquakes.
Earthquakes happen when under the ground rocks break at a fault. The rocks then break it release of energy which causes semi waves.
When waves approach a rocky headland, they are forced to change direction and refract around the obstacles. This change in direction causes an increase in wave energy and pressure on the headland, resulting in erosion and the release of energy as the waves crash against the rocks. The energy is dissipated as the waves break, causing erosion and shaping the coastline over time.
Seismic waves (like all waves) transmit energy.
The release of energy stored in deformed rocks is known as an earthquake. This occurs when the built-up stress within the rocks is released suddenly along a fault line, causing seismic waves to propagate through the Earth's crust.
they release all their built up energy in the form of shock waves