What is the primary mineral structure of Chrysotile?

Chrysotile, also known as asbestos, is classified as a member of the serpentine group of minerals. Its unique structure consists of layered sheets of magnesium silicate, which gives it flexibility and allows it to be easily woven into fabrics, a characteristic that distinguishes it from other forms of asbestos. The serpentine structure contributes to its different physical properties, such as its ability to resist heat and chemical damage while remaining pliable. These attributes are significant in various industrial applications, although they also present specific health risks when inhaled. Understanding that chrysotile belongs to the serpentine family is crucial in recognizing its properties and the precautions necessary when handling it.