Generically, they are called "rime". Primary constituents are salt, with other solutes being metal oxides and such.
1) Ocean water seeps down through cracks in the crust. 2) Water comes in contact with magma that heats it to a very high temperature. 3) The heated water then dissolves minerals from the crust and rushes upward. 4)The solution billows out of chimneys. When the solution hits the sea, minerals crystallize on the ocean floor.
Carbon Dioxide dissolves in ocean water. Plants in the ocean use the carbon dioxide dissolved in the ocean water.
Taste due to the type of minerals dissolved in the water
It is called Leaching
Oceans are big water bodies. Salinity is due to the presence of minerals in water.
The minerals and dissolved gases in ocean water are used by plant and animals.
These minerals are dissolved in the water while it moves through the earth.
Mineral deposits are formed when ground water that contains dissolved minerals are cooled or has evaporated. Some of these mineral deposits are iron ions, magnesium, and calcium.
halite deposits
Halite deposits.
Superheated water forces its way into rock faults. It contains many dissolved minerals which crystallise out when the water cools.
halite deposits
Continental Erosion
Ocean water has many more various salts and minerals dissolved in it.
Dissolved minerals are usually in the form of ions. Therefore water that is free of dissolved minerals is called deionized water.
Because the water they are using contains high concentrations of dissolved minerals, these are left behind when the water boils
There is a lot of water on earth. A lot of it. And it is continually recycled. It has a tendency to wash anything that is water soluble into the ocean, where it remains dissolved as the water cycle continues. This has been happening for millions and millions of years, and a lot of water soluble minerals have been dissolved in seawater over that time.In contrast, we can find water soluble minerals in dry regions. In places where it is extremely arid, there is so little precipitation that the water soluble minerals haven't been dissolved and washed away like they have been in other regions.