Waves crash on the shore when they approach shallow water, causing the wave height to increase and eventually break. This is due to the friction between the rising wave and the ocean floor, which slows down the bottom of the wave and causes the top to topple forward, forming a breaking wave.
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When waves crash against the shore, they appear as foamy, white crests that break and dissipate as they hit the land.
Waves crash when the energy in the wave becomes too concentrated as it approaches the shore. This causes the top of the wave to move faster than the bottom, resulting in the wave breaking. The forceful impact of the crashing wave is what we see and hear as it hits the shore.
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Near shore crest shaped waves are called "plunging waves." These waves are characterized by a curling crest that breaks forward as the wave approaches the shore.
A wavefront is an imaginary surface representing corresponding points of a wave that are in phase. It can also be seen as the boundary of a wave in which the points on the wave are all in the same phase. This can be used to describe light waves, sound waves, or any other type of wave.