Phyllosilicates

Phyllosilicates are a group of minerals characterized by their layered structure, composed primarily of silicon and oxygen, along with other elements like aluminum and magnesium. These minerals can be found in various rocks and are known for their sheet-like formation, which allows them to easily split into thin flakes. Common examples include mica and clay minerals. Phyllosilicates play essential roles in soil formation, plant growth, and various industrial applications, including ceramics and paints, due to their unique physical and chemical properties. Their ability to retain moisture also makes them vital in agriculture.