A wave cut platform is formed when the destructive waves hit the face of the cliff and cause undercutting between the high and low tide marks. This is a result of corrosion and hydraulic action it is called a wave-cut notch and the part of cliff above is called the overhang . This notch gets bigger over time and creates a small cave under the cliff. The overhang will eventually become unsupported and then it will collapses and the cliff begins to retreat. The boulders from the cliff will be carried away by the sea and will uncover a gently slopping wave-cut platform. As this process repeats itself the wave-cut platform will increase in size as the cliff retreats further. At high tide the wave-cut notch will slowly become smoother from erosion such as solution, attrition and corrosion although it will still have rock pools.
by Evie5287
Wave cut platforms are found along coastlines where there are cliffs or other elevated landforms being eroded by the action of waves over time. These platforms are typically located in areas with high wave energy and are commonly seen in coastal regions with rocky shorelines.
An incipient wave is a wave that is just beginning to form. It is in the early stages of development and has not fully developed into a mature wave with a well-defined shape and crest.
Notches are formed through the process of erosion, where the repeated action of water or wind gradually wears away rock layers to create a narrow indentation or groove. This erosion can be caused by factors like wave action on coastlines, flowing rivers, or glacial movement. Over time, the continuous abrasion of the rock surface deepens and widens the notch.
A "tsunami" is not a land form, it is a wave.
An example of a transverse wave is a wave on a string when it is plucked or shaken. In this type of wave, the particles of the medium move perpendicular (sideways) to the direction of the wave propagation. This causes crests and troughs to form as the wave travels along the medium.
sea defenses have been built to protect it from erosion such as longshore drift and wave cut notches
Wave erosion can create features such as sea cliffs, sea stacks, wave-cut platforms, caves, and arches along coastlines. These features form as a result of the continuous force of waves breaking against the shoreline and eroding the rock over time.
The past form of "wave" is "waved."
Electromagnetic wave
Wave-cut platforms are formed through erosion by the action of waves pounding against the coastline. As the waves erode the base of the cliffs, a gently sloping platform is created over time.
A saw tooth wave form superimposed over a square wave form is TPZi wave form. Most of the Inverters use this technology instead of pure sine wave form of out put.
A wave front has a form that is a surface of a sphere.
Wave cut platforms are found along coastlines where there are cliffs or other elevated landforms being eroded by the action of waves over time. These platforms are typically located in areas with high wave energy and are commonly seen in coastal regions with rocky shorelines.
seacaves,seasticks,wave-cut platforms and more
Electromagnetic wave
Rivers can erode valleys, create meanders, and form river cliffs. Coastal erosion can result in the formation of sea cliffs, wave-cut platforms, and sea caves.
The P-wave which is a form of body wave known as a compression or longitudinal wave.