Quartz and Feldspar are the two common minerals in the earths crust
Quartz is hard white or colorless mineral consisting of silicon dioxide, found widely in igneous metamorphic, and sedimentary rocks. It is often colored by impurities.
Feldspar is an abundant rock froming mineral typically ocurring as colorless or pale colored crystals and consisting of alluminosilicates of potasium, sodium, and calcium