It is a process known as shoaling. When waves feel the bottom they slow down and decrease their wavelength but the period of the waves does not change. The height of the wave will steadily increase until the wave becomes unstable and breaks near the beach.
the wave builds up and crashes on the shore
like it will first do something than another...thing......... i guess.................................♥
true
Waves shape a beach by eroding the shore in some places and building it up in others. ♥
If the Coast Guard warns of a giant wave of water approaching the shore as a result of a major earthquake, they are warning of...... a tsunami
Waves even out a shoreline by eroding it.The waves coming to shore gradually change direction, as different parts of the wave begins to drag the bottom.The energy of the wave is concentrated on headlands, part of the shore that sticks out into the ocean.As waves erode the headlands the shoreline will eventually even out.Tee Hee!!!!!!!!!!!!!!!!!!!!!!!! ___------ -/---- ----\/--- --- \------------ ---- --
waves occur all the time but after an earthquake tidal waves occur. Tidal waves are the cause of the tectonic plates colliding underwater. After the collision over time the wave goes form a small bump in the water to growing bigger and bigger into giant super wave capable of destroying towns.
The wave would slow down as it approaches the shore.
The wave would slow down as it approaches the shore.
Breakercrest
It is aclled an high tide
Of course it can. That is why some waves don't reach the shore.
Ocean water within a wave moves in a circular motion in open water. As the wave approaches the shore, the water becomes shallow and the bottom.
true
Depending on height at origin as it approaches the coastal shelf it will rise and increase the strength of the wave. for example a wave 50ft high approaching the atlantic coastal shelf could rise to 150-200 feet with disastrious ramifications.
because earth is moving and when we move sometimes mostly everything moves with earth and it goes different ways everyday of an year
As it approaches the shore the energy moving through the water meets the shallows resistance. It collapses into the wave you see at the beach. This energy can smooth out the beach with the help of tidal variation. Make rocks into sand.
Depending on height at origin as it approaches the coastal shelf it will rise and increase the strength of the wave. for example a wave 50ft high approaching the atlantic coastal shelf could rise to 150-200 feet with disastrious ramifications.
Laminar flow compession