Silicates
Silicates are a large and diverse group of minerals that are based on the silicate tetrahedron (SiO4)4- unit, which consists of a silicon atom bonded to four oxygen atoms. The silicate tetrahedra are linked together in various ways to form different types of structures, resulting in a wide range of silicate minerals with different physical and chemical properties. Silicates are the most abundant minerals on Earth, making up over 90% of the Earth's crust. They are also found in many other natural materials, such as rocks, soils, clays, and sands, as well as in many synthetic materials, such as glass and ceramics.
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