Minerals are naturally occurring, inorganic solid compounds characterized by a crystalline structure. In physical sciences, they are fundamental components of the Earth's crust, forming through various geological processes such as precipitation, metamorphism, and crystallization. From a chemical and biological perspective, minerals represent essential elemental building blocks; these elements are critical in biological systems for maintaining structural integrity and facilitating biochemical reactions. Their importance spans structural support in biological matrices and participation in enzymatic pathways. The properties of minerals, including hardness, crystal lattice, and chemical composition, are governed by atomic bonding and the thermodynamic stability of the compound under natural conditions.