Gypsum. Also consider Halite.
Rocks composed of evaporite minerals, such as halite and gypsum, are rocks formed by evaporation of fluids.
Evaporation of a sodium chloride (NaCl) solution.
Gypsum is an extrusive sedimentary rock formed from the evaporation of seawater.
From biological processes: organic sedimentary rock.From precipitation or evaporation: chemical sedimentary rock.
first of all rocks don't evaporate. Second of all they turn into magma then when magma cools it turns into igneous rock
Three rocks that form from precipitation or evaporation include limestone, rock salt, and gypsum. Limestone is formed from the accumulation of calcite precipitated from water. Rock salt is formed by the evaporation of salty water, leaving behind salt crystals. Gypsum forms when water evaporates from a mixture of calcium, sulfur, and oxygen.
Sedimentary rock formed from water evaporation is known as evaporite. This type of rock is created when bodies of water, such as lakes or seas, experience evaporation, leading to the precipitation of dissolved minerals. Common examples of evaporites include rock salt (halite) and gypsum, which form as the water concentration increases and the minerals crystallize out of the solution. These rocks often indicate past environmental conditions where water was abundant and subsequently dried up.
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.
Most rock gypsum is formed by the evaporation of seawater in shallow marine environments. As water evaporates, it leaves behind dissolved minerals, including calcium sulfate, which crystallizes to form gypsum. This process can occur in lagoons or arid regions where evaporation rates are high. Over time, accumulated gypsum deposits can be compacted and lithified into rock gypsum.
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.
Dolostone is formed through the replacement of calcium ions in limestone with magnesium ions, a process known as dolomitization. Rock gypsum is formed through the precipitation of minerals from evaporating water, leaving behind gypsum deposits.
Borax rock is formed through the evaporation of water in arid regions, such as dry lake beds or hot springs. As the water evaporates, minerals like borax are left behind, eventually forming a solid crystalline structure known as borax rock.