Potash / Soda Feldspar

Potash Feldspar is a largely abundant group of minerals in the earth’s crust, which forms around 60% of available terrestrial rocks. The deposits provided sodium feldspar and potassium feldspar with mixed feldspars. Feldspar minerals are an indispensable component in igneous, metamorphic and sedimentary rocks, to such a level that the arrangement of a number of rocks having a base with required feldspar content. The mineralogical composition of most feldspar can be articulated in terms of the ternary system Orthoclase, Albite as well as Anorthite.