it doesnt
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Oh yes it does!
Calcium carbonate (main constituent of limestone), magnesium carbonate (ditto of dolomite), calcium sulphate (gypsum), sodium chloride ("ordinary" table salt, but in its rock form), and some other metallic compounds, can all be dissolved by groundwater derived directly from rain and snow-melt.
Hot, high-pressure (hydrothermal) water is mroe aggressive and will leach more metallic salts from granite etc.
The dissolved minerals may then be deposited elsewhere by evaporation.
Minerals deposited by water are known as evaporites. These minerals are formed when water evaporates and leaves behind dissolved minerals that then precipitate out of the solution and accumulate. Examples of evaporite minerals include halite (salt), gypsum, and calcite.
Water must evaporate or cool down in order for its dissolved minerals to be deposited. As the water evaporates or cools, it becomes supersaturated with minerals, causing them to come out of solution and form solid deposits. This process is known as precipitation.
Placer deposits. These are formed by the settling of heavy minerals like gold, diamond, and platinum when the energy of the river current decreases, allowing the denser particles to sink to the bottom.
Minerals in placer deposits come from the erosion and weathering of rocks and minerals in the surrounding areas. These minerals are carried by water and eventually deposited in rivers, streams, and beaches where they settle due to their weight. The concentration of minerals in placer deposits can vary depending on the geology of the region.
The minerals formed in narrow channels or slabs of rock are called vein minerals. These minerals are deposited within the fractures of the rock, often in a crystalline form. They can include a variety of minerals such as quartz, calcite, and sulfides.
Soil rich in minerals deposited by flooding rivers is called silt.
Sedimentary
Minerals deposited by water are known as evaporites. These minerals are formed when water evaporates and leaves behind dissolved minerals that then precipitate out of the solution and accumulate. Examples of evaporite minerals include halite (salt), gypsum, and calcite.
The term would be 'precipitated'.
Osteoblasts.
Shell, bone, a reef.
Water must evaporate or cool down in order for its dissolved minerals to be deposited. As the water evaporates or cools, it becomes supersaturated with minerals, causing them to come out of solution and form solid deposits. This process is known as precipitation.
Placer deposits. These are formed by the settling of heavy minerals like gold, diamond, and platinum when the energy of the river current decreases, allowing the denser particles to sink to the bottom.
Alluvial soil is the soil that is deposited by flooding. It is characterized by its high fertility due to the minerals and nutrients it receives from the floodwaters.
Osteoblasts are the bone cells responsible for secreting a substance called osteoid, which is a matrix made up of collagen and other proteins. This osteoid provides the scaffold where minerals, such as calcium and phosphate, are deposited to form solid bone tissue.
Soil deposited by water could be silt or mud.
Minerals in placer deposits come from the erosion and weathering of rocks and minerals in the surrounding areas. These minerals are carried by water and eventually deposited in rivers, streams, and beaches where they settle due to their weight. The concentration of minerals in placer deposits can vary depending on the geology of the region.