Inosilicates are a group of silicate minerals characterized by their unique chain-like structures. These minerals consist of silicate tetrahedra linked together in one-dimensional or two-dimensional chains. The chains can vary in length and can be single or double, leading to different types of inosilicates, such as pyroxenes and amphiboles. Inosilicates are commonly found in igneous and metamorphic rocks and play a significant role in geology. They are important for understanding the formation and evolution of the Earth's crust. Their properties, such as hardness and cleavage, make them valuable in various industrial applications, including ceramics and construction materials.