Marble is a stone coming about because of changeability of sedimentary carbonate rocks, most ordinarily limestone or dolomite shake. Transformative nature causes variable recrystallization of the first carbonate mineral grains. The subsequent marble shake is ordinarily made out of an interlocking mosaic of carbonate gems. Essential sedimentary surfaces and structures of the first carbonate shake (protolith) have ordinarily been changed or pulverized.

Unadulterated white marble is the aftereffect of transformative nature of an extremely unadulterated (silicate-poor) limestone or dolomite protolith. The trademark whirls and veins of kaleidoscopic marble assortments are typically because of different mineral contaminations, for example, dirt, residue, sand, iron oxides, or chert which were initially present as grains or layers in the limestone. Green hue is frequently because of serpentine coming about because of initially magnesium-rich limestone or dolomite with silica debasements. These different polluting influences have been assembled and recrystallized by the extraordinary weight and warmth of the transformative nature.