The force that acts on an ocean wave as it nears the shore is called shoaling. Shoaling is the process where the wave interacts with the seafloor, causing the wave to slow down and increase in height. This is what causes waves to break as they approach the shore.
The force of friction between the ocean wave and the sea floor causes the wave to slow down as it nears the shore. This frictional force results in the wave increasing in height and eventually breaking as it reaches shallow water.
A dumping wave is a type of ocean wave that breaks quickly and powerfully, with a lot of force towards the shore. It creates a steep, crashing wave face that can be dangerous for swimmers and surfers.
The force of friction between the wave and the seabed as the wave approaches the shore causes it to slow down and increase in height. This interaction, known as wave shoaling, leads to changes in the wave's characteristics, such as height, speed, and steepness.
because when a wave breaks onto the shore it gets sucked back into the ocean where the wind will turn it into a new wave, or swell.
Movement of the ocean, or tides are directly related to deep ocean currents. Deep ocean currents are also responsible for the wind that causes the waves to crash into the shore.
WHEN THE OCEAN WASHES farther up on shore
The Atlantic Ocean is on Florida's eastern shore.
The rocky part of the shore that sticks out in the ocean is called a jetty.
Manifest Destiny describes the US Colonial belief that settlers had the right and should expand from shore to shore, from the Atlantic Ocean to the Pacific Ocean.
they do more damage to the shore
The Atlantic Ocean.