The water level by the rock was raised by the wave, causing it to hit the rock with more force. This could lead to erosion of the rock over time if the waves continue to impact it.
The wave caused the water level to rise and fall as it passed by the rock. This change in water level is a result of the wave's energy moving through the water.
The size of a wave is not affected by the wavelength, but rather by the energy carried by the wave. The wavelength determines the distance between wave crests, while the amplitude of the wave determines its size or height. Changing the wavelength of a wave will not inherently change its size.
When a wave approaches shallow water, its height increases, and there is a tendency for the wave to slow down and eventually break. This is due to the decrease in water depth, causing the wave energy to become more concentrated.
The crest is at the top of a wave, the trough is at the bottom of the wave.
The highest point of a transfer wave is called the crest. It is the peak of the wave where the water is at its highest level.
The water level by the rock will rise as the wave approaches, then fall as the wave passes by, creating a temporary increase and decrease in water height. The closer the rock is to the wave action, the more significant the water level fluctuations will be. Additionally, factors such as wave height, frequency, and rock shape can influence how the water level changes.
The water level on the rock is influenced by the wave's energy and height. When a wave crashes onto the rock, it displaces water, temporarily raising the water level around it as the wave breaks and flows over the surface. As the wave recedes, the water level drops again, often leaving behind a thin layer of water that may evaporate or drain away. This cyclical process continuously alters the water level on the rock with each passing wave.
The wave caused the water level to rise and fall as it passed by the rock. This change in water level is a result of the wave's energy moving through the water.
The water level by the rock would have significantly risen due to the influx of water from the tsunami waves. Tsunamis are known for causing a rapid and massive rise in water levels along coastlines, resulting in flooding and inundation of low-lying areas.
The water molecules of a deep-water wave move in a circular motion. The diameter of the motion decreases with the distance from the surface. The motion is felt down to a distance of approximately one wavelength, where the wave's energy becomes negligible.
The water part :) Hope this helps.
The landform is called a wave-cut cliff, or wave-cut platform, where a flat rock area extends into the sea, at or near the water level.
The size of a wave is not affected by the wavelength, but rather by the energy carried by the wave. The wavelength determines the distance between wave crests, while the amplitude of the wave determines its size or height. Changing the wavelength of a wave will not inherently change its size.
When a wave approaches shallow water, its height increases, and there is a tendency for the wave to slow down and eventually break. This is due to the decrease in water depth, causing the wave energy to become more concentrated.
A wave ;D
the amplitude of a water wave is the maximum distance a water particle moves above or below the surface level of calm water.
The crest is at the top of a wave, the trough is at the bottom of the wave.