MINERALS – Metamorphic

Metamorphic minerals are formed when rocks are subjected to high temperatures and pressures deep within Earth's crust. These minerals exhibit unique crystal structures and compositions, often with striking colors and patterns. The process of metamorphism can alter the chemical composition of existing minerals, creating new ones. Examples of metamorphic minerals include garnet, staurolite, and kyanite, which form in specific geological settings. Metamorphic rocks, like marble and slate, often contain characteristic mineral assemblages that indicate their formation history.