Potassium feldspar, often called K‑feldspar or potassic feldspar, is a group of important rock‑forming minerals that contain potassium, aluminum, and silica. It is one of the most abundant minerals in the Earth’s crust and is commonly found in igneous and metamorphic rocks such as granite. Potassium feldspar is widely used in ceramics, glass production, and as a flux in various industrial processes because it lowers melting temperatures and improves material strength.