Minerals that crystallize directly from seawater are examples of hydrogenous sediment.
hydrogenous sediment
The hot magma heats the ocean water that seeps underground. The heated water dissolves minerals. When the solution billows out of vents called "chimneys" the minerals crystallize in the cold sea water. I hope that answers your question ^^
The density of seawater increases if salinity increases.
97% seawater, other 3% is freshwater.
274g seawater x 3.5gNaCl/100g seawater =9.6g NaCl
hydrogenous sediment
not a hydrogenous sediment?
Hydrogen, oxygen, trace minerals.
Mineral formation can occur several ways along the MOR. Rising magma can cool and crystallize, forming igneous rock which contains various minerals. Heated seawater also percolates through the hot rock of the MOR, and can precipitate minerals on rock surfaces and at black smokers.
potassium and sulfate
Desalination
The hot magma heats the ocean water that seeps underground. The heated water dissolves minerals. When the solution billows out of vents called "chimneys" the minerals crystallize in the cold sea water. I hope that answers your question ^^
Chemical sedimentary rock is created by precipitation of minerals out of, or evaporation from, saturated solutions that are high in dissolved minerals. Rock gypsum and rock salt are two examples.
The term is Desalination.
Air, seawater.
Seawater contains salts as well as other minerals in its suspension, therefore it is hypertonic to drinking water.
Manganese nodules do not accumulate below 4500 meters depth because the manganese minerals are highly soluble in seawater below that depth.