The Relationship between the relief of an area and the contour interval on a map of the area is A contour line
The ocean as a whole is pulled in the direction of the moon, by the moon's gravitational field (the sun also has a tidal effect, although smaller). So water pulled away from an area of low tide is pulled toward an area of high tide.
Without the earth's rotation, the only natural force controlling oceanic activity would be gravity. The sun and the moon would provide only a minor contribution to ocean behavior because of their distance to the earth. Ocean water would instantly attract towards the part of the earth where the center of the strongest gravity pull is taking place. Tides would centralize to this area and disturbed only by catastrophic weather phenomenon that may be provoked by climatic changes do to the lack of rotation.
tides periodically rise and fall on the water level of the ocean and waves move in an up-and-down motion along the surface of a body of water
Gypsum is formed underwater, usually between layers of shale and limestone. When the water evaporates and the area dries, the gypsum becomes solid "rock" gypsum.
The area between bulges of water in the ocean is known as a trough. This is the part of the water surface that is lower between two adjacent crests. Troughs are typically found in waves and result from the alternating rise and fall of the water.
The area between bulges of water is a depression or a low-tide area. High tidal bulges have these low-tide areas which would correspond to troughs.
Ocean bulges are caused by gravitational forces from the Moon and Sun. These forces create a slightly elevated area of water in certain parts of the ocean, resulting in bulges that lead to phenomena like tides.
Tidal pools are formed when water is drawn away from an area between high tides.
a spit
Places on Earth between tidal bulges experience a decrease in water level or low tide. This occurs when the gravitational force of the Moon and the Sun pull the water towards them, causing a bulge on each side, leaving the area in between with lower water level.
You would find the foreshore between the berm and the water. This area is affected by the tides and waves and is commonly where beachgoers spend their time.
A tidal pool is formed when water is drawn away from the intertidal zone during low tide, leaving a shallow pool of water behind. These pools can support a variety of marine life until the tide returns and replenishes them with ocean water.
It is called the tidal plain.
An area will experience 2 High tides and 2 low tides
A beach or foreshore could be formed between the high and low water marks. This area typically experiences the deposition of sand, gravel, and other sediments carried by waves and tides.
an area where rivers rise and fall with ocean tides