In a restricted ocean as opposed to a closed ocean, as the restricted ocean evaporates, more salty water enters from outside. This continuously replenishes the salt that is being deposited allowing for thick evaporate layers to form. Many examples actually show that the new water episodically enters the evaporating ocean.
The original concentration of dissolved minerals in a restricted ocean basin was enough to form only a thin evaporated layer. As the restricted ocean evaporates, more salty water enters from outside and continuously replenishes the salt that is being deposited allowing for thick evaporate layers to form.
This is known as an evaporite, examples include Halite, Gypsum and certain types of Limestone.
Halite is an evaporite mineral, meaning it forms as a result of evaporation from concentrated liquid solutions containing dissolved minerals.
Some limestones are made by precipitation of dissolved calcium carbonate. Some cherts are formed from dissolved silicates in thermal springs and evaporite minerals, such as gypsum and rock salt (halite) are formed by evaporation of water from solutions of dissolved minerals.
Conglomerate is a sedimentary rock composed of rounded gravel-sized particles, while evaporite is a sedimentary rock formed from the precipitation of minerals that were dissolved in water. Conglomerate forms from the erosion and transportation of pre-existing rocks, while evaporite forms through the evaporation of water. Both rocks can contain a variety of minerals and can provide clues about the environment in which they formed.
Halite and gypsum are two examples of evaporite minerals.
Evaporite minerals are water-soluble mineral sediments that were formed from precipitation. The three common evaporite minerals are gypsum, anhydrite and halite.
Some limestones are made by precipitation of dissolved calcium carbonate. Some cherts are formed from dissolved silicates in thermal springs and evaporite minerals, such as gypsum and rock salt (halite) are formed by evaporation of water from solutions of dissolved minerals.
Rock gypsum and rock salt are two examples of sedimentary evaporite rocks.
Evaporite minerals are minerals found in sedimentary rocks that are formed as precipitates from the evaporation of a saline solution. A diapir structure formed by evaporite minerals is a salt dome.
This forms in bodies of water in which water evaporates faster than it is receiving rain. (This process is called precipitation) This causes the minerals in the water to be left behind, in which they become a rock. (An evaporite) examples of an evaporite is Gypsum.
Rock Salt
It is not a rock but an evaporite mineral.