Notch
Well a V-notch gives better accurate results when compared to rectangular notch.
The creator of minecraft is a man who is commonly called "Notch", his real name is Markus Persson He created minecraft from scratch and now he has formed mojang the company to help him, he makes many games and often enters in game contests.
No notch is still alive
There is no such thing. It is a word that is sometimes accidentally used when referring to the suprasternal notch, which is also known as the jugular notch.
A wave-cut notch is a notch or recess in a coastal cliff formed by the erosion from wave action, typically at the high tide mark. It is created as waves constantly wear away the base of the cliff, leading to a recession in the rock face. Overtime, the wave-cut notch can develop into a larger feature such as a sea cave or sea stack.
waves
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 CLIFF, WAVE-CUT TERRACE or PLATFORM, SEA NOTCH, SEA CAVES, SEA ARCH, AND SEA STACK!
WAVE-CUT CLIFF, WAVE-CUT TERRACE or PLATFORM, SEA NOTCH, SEA CAVES, SEA ARCH, AND SEA STACK!
wave cut cliffs are formed by wind and tide driven waves
Cliffs are formed when erosion is greatest when large waves actually break against the foot a cliff. The foot of the cliff is undercut to form a wave cut notch. As the notch gets larger, the cliff above it will become increasingly unsupported and in time will collapse. As this process is repeated the cliff will slowly retreat and, usually, increase in height. The gently sloping land left at the foot of the retreating cliff is called a wave cut platform.ITS SNOWING YH THTSBRITEEEEEEEEEExX-I2uN-ReiSS-Xx add my psn
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
A wave-cut notch is caused by the erosive action of waves pounding against a cliff face over time, leading to the formation of a horizontal groove at the base of the cliff. This erosion is primarily driven by hydraulic action and abrasion, as waves carry sediment and debris that wear away the rock surface.
wave-cut terrances
A wave-cut platform is the narrow flat area often seen at the base of a sea cliff caused by the action of the waves. It forms after destructive waves hit against the cliff face, causing undercutting between the high and low water marks, mainly as a result of corrosion and hydraulic power, creating a wave-cut notch. This notch then enlarges into a cave. The waves undermine this portion until the roof of the cave cannot hold due to the pressure and freeze-thaw weathering acting on it, and collapse, resulting in the cliff retreating landward.
A headline deck is formed when waves cut completely through a headline. This occurs when a wave has a significant portion of its energy intersected by the shoreline.