Marble slabs / tiles
Marble is formed from limestone by heat and pressure in the earth?¯s crust. These forces cause the limestone to change in texture and makeup. This process is called recrystallization. Fossilized materials in the limestone, along with its original carbonate minerals, recrystallize and form large, coarse grains of calcite. Impurities present in the limestone during recrystallization affect the mineral composition of the marble that forms. At relatively low temperatures, silica impurities in the carbonate minerals form masses of chert or crystals of quartz. At higher temperatures, the silica reacts with the carbonates to produce diopside and forsterite. At extremely high temperatures, rarer calcium minerals, such as larnite, monticellite, and rankinite, form in the marble. If water is present, serpentine, talc, and certain other hydrous minerals may be produced. The presence of iron, alumina, and silica may result in the formation of hematite and magnetite.
Marble has been valued for thousands of years for it's rich palette of colors. Marble is however more porous than granite. For this reason, we highly recommend that you NOT put marble in the kitchen. Marble stones consist of limestone that has undergone heat and pressure. A transformation process takes place when the weight of overlying material, pressure from crystal collisions and heat from the earth's core generate temperatures in excess of 1800ºF. Texture of marble depends on the form, size and uniformity of grains. The element components of marble determine the color of the stone. Generally calcite and dolomite marbles are of pure white color. Variations of whiteness of pure marbles are due to the mixture of foreign substances. Such impurities form streaks and clouds. White Cabrera, Emperador Dark, Alabama White, Crema Valencia.
