A mineral.
The mineral chalcanthite is composed of hydrous copper sulfate. It is translucent and a rich blue in color. Chalcanthite has a hardness of 2.5. The oxidation of copper sulfides is what causes it to form in nature.
Lab-created chalcanthite is not inherently toxic, but it is important to handle it with care as it can irritate the skin and eyes. It is advised to wear gloves and avoid ingesting or inhaling the substance.
Chalcanthite is commonly found in arid and semi-arid regions, often associated with copper deposits. It typically forms in oxidized zones of copper-bearing minerals, especially in areas where copper sulfides are present. Notable locations include the United States (particularly in Arizona and New Mexico), as well as parts of Chile, Morocco, and Germany. It can also be found in evaporative environments, where it crystallizes from solutions containing copper.
Copper sulphate found naturally in the Earth's crust is typically in the form of chalcanthite.
It becomes a non-crystalline, powdery anhydrous salt.The hydrated (pentahydrate) form is chalcanthite, a bright blue crystal. The rare anhydrous ore form is called chalcocyanite, a gray or pale-green powdery rock.(If heated to 650 °C, copper sulfate becomes copper oxide and sulfur trioxide.)
It becomes a non-crystalline, powdery anhydrous salt.The hydrated (pentahydrate) form is chalcanthite, a bright blue crystal. The rare anhydrous ore form is called chalcocyanite, a gray or pale-green powdery rock.(If heated to 650 °C, copper sulfate becomes copper oxide and sulfur trioxide.)
From Wikipedia:Copper(II) sulfate is the chemical compound with the formula CuSO4. This salt exists as a series of compounds that differ in their degree of hydration. The anhydrous form is a pale green or gray-white powder, whereas the pentahydrate, the most commonly encountered salt, is bright blue. The anhydrous form occurs as a rare mineral known as chalcocyanite. The hydrated copper sulfate occurs in nature as chalcanthite (pentahydrate), and two more rare ones: bonattite (trihydrate) and boothite (heptahydrate). Archaic names for copper(II) sulfate are "blue vitriol" and "bluestone".[1]
A mineral sulfate is a type of mineral that contains the sulfate ion (SO42-). Sulfate minerals are found in many different environments, including evaporite deposits, hydrothermal veins, and the oxidizing zone of sulfide mineral deposits. Some common examples of mineral sulfates include: Barite (BaSO4) Celestite (SrSO4) Anglesite (PbSO4) Anhydrite (CaSO4) Gypsum (CaSO4·2H2O) Chalcanthite (CuSO4·5H2O) Epsomite (MgSO4·7H2O) Sulfate minerals are used in a variety of applications, including: The manufacture of fertilizers and other chemicals The production of cement and plaster The extraction of metals The treatment of water The use as a food additive Sulfate minerals are generally non-toxic, but some can be harmful if ingested in large quantities. For example, barite can cause respiratory problems, and celestite can cause kidney damage. Here are some of the properties of mineral sulfates: They are typically white, colorless, or pale yellow in color. They have a Mohs hardness of 2 to 3, which means that they are relatively soft. They are often transparent or translucent. They have a distinctive luster, which can be vitreous, pearly, or earthy. Sulfate minerals are an important part of the Earth's crust, and they have a variety of uses in the modern world.