Chlorite is a group of minerals that are typically green in color and are part of the phyllosilicate family. These minerals are composed mainly of magnesium, iron, and aluminum silicate, and they often form in metamorphic rocks. Chlorite is known for its layered structure, which gives it a flaky appearance and allows it to easily split into thin sheets. Chlorite is commonly found in environments where metamorphism occurs, such as in schist and slate. It can also be present in some igneous rocks and is often associated with other minerals like mica and serpentine. Due to its unique properties, chlorite is used in various industrial applications, including ceramics and as a filler in paints.