Following oxygen and silicon, the third most abundant element in the Earth's crust by mass is aluminum. Comprising a significant portion of the Earth's solid outer layer, aluminum contributes to the diverse mineral composition of the crust. Its prevalence is notable in various minerals and rocks, such as feldspars and bauxite, reflecting its integral role in geological processes. Beyond its geological significance, aluminum holds practical importance in industrial applications and daily life due to its lightweight, durable, and corrosion-resistant properties. Understanding the distribution of elements in the Earth's crust is essential for unraveling the complex dynamics that have shaped our planet over geological time scales.