Mineral classification is the systematic organization of minerals based on their chemical composition and crystal structure. Minerals are typically categorized into groups such as silicates, carbonates, and oxides. Each group shares similar properties and characteristics, making it easier for scientists to study and identify them. The most common classification system is the one developed by the International Mineralogical Association, which divides minerals into categories based on their dominant anions. This classification helps in understanding the relationships between different minerals and their formation processes, aiding in fields like geology and materials science.