How is it formed?
Egyptian marble undergoes a remarkable journey through geological ages to attain its exquisite form. It originates from eroded rocks like limestone, accumulating as sedimentary layers in water bodies. Over time, the weight of overlying sediments compresses the layers, facilitating the precipitation of minerals carried by groundwater. As minerals crystallize, sediment particles bind together through cementation. Subsequent burial leads to metamorphism, wherein heat and pressure cause minerals to recrystallize, transforming the rock into marble. The incorporation of impurities contributes to its distinctive colors and veining. Geological forces then uplift and expose marble-rich layers, enabling quarrying. Read More