This is an example of refraction, as the waves are being turned from their original path. This can result in the formation of a longshore (parallel) current that flows seaward as a "rip tide."
This process is called wave refraction. It occurs as waves approach the shoreline and the part of the wave in shallower water slows down, causing the wave to bend and align parallel to the shore.
When waves tend to become parallel to the shore, it is called wave refraction. This occurs as waves change direction and bend towards the shore due to variations in water depth, causing them to align parallel to the shoreline.
The process is called wave refraction. As deep water waves enter shallow water, the portion of the wave closest to the shore slows down due to the shallower depth, causing the wave to bend and align more parallel to the shoreline. This phenomenon helps reduce the wave energy hitting the shore more directly.
The process is called canonization.
A shallow area may be called a "ford" (the verb to fordis "to cross at a shallow point").
a small, shallow dish
When ocean waves reach shallow water, their speed decreases and their height increases. This process is called wave shoaling. The wave energy is forced to compress, causing the waves to break and become steeper before crashing onto the shore.
Shallow parts of the sea or ocean are called shoals or shallows. They are areas where the water depth is relatively shallow, making them potentially hazardous for navigation.
That "mystical process" is called transubstantiation.
Process is called naturalization.
The process is called bidirectional replication. In this process, DNA polymerases synthesize new strands in opposite directions on each template strand.
Yes it can. this process is called condensation.