Clinozoisite is a mineral belonging to the epidote group, primarily composed of calcium, aluminum, and silicate. It typically forms in metamorphic rocks and is characterized by its green to yellow-green color, often exhibiting a glassy luster. Clinozoisite can be found in various geological environments, particularly in regions with high-pressure and high-temperature conditions. This mineral is often associated with other minerals such as epidote and garnet. Clinozoisite is important in geology as it helps scientists understand the conditions under which certain rocks formed. Its unique properties make it a subject of interest for mineral collectors and researchers alike.