The Earth's crust is the thin, outermost solid layer of our planet which forms both the continents and the ocean floors. It lies above the mantle and makes up less than 1% of Earth's total volume but it is the most accessible and studied layer because all landforms, soils and rocks we see are part of the crust. The crust is composed mainly of solid rocks and minerals, which in turn are made from various chemical elements. These elements do not exist in pure form but are combined in complex compounds like silicates, oxides, carbonates etc. Although more than 90 naturally occurring elements are found in the crust, only a small group of them dominate its total mass. The composition of the crust reflects its geochemical origin, its formation history and the processes like weathering, erosion, and plate tectonics that continuously shape it. Each of these elements has specific roles in rock formation and Earth’s surface structure. Their proportions are usually expressed by mass pe...