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  2. Polished plaster - Wikipedia

    en.wikipedia.org/wiki/Polished_plaster

    A lime-based polished plaster may contain over 40% of marble powder. [2] Polished plaster is mainly used internally, on walls and ceilings, [3] to give a finish that looks like polished marble, travertine, or limestone. Such plasters are usually applied over a primer and basecoat base, from one to four layers.

  3. 30 White Bathroom Ideas That Are Bright and Beautiful - AOL

    www.aol.com/white-bathroom-designs-anything...

    Here, Krisitin Kostamo-McNeil of Anne Rae Design tiles the lower half of the wall with white tiles, adding in a few black stripes. There's also a black-and-white pebble floor and a black marble ...

  4. Tile - Wikipedia

    en.wikipedia.org/wiki/Tile

    Granite or marble tiles are sawn on both sides and then polished or finished on the top surface so that they have a uniform thickness. Other natural stone tiles such as slate are typically "riven" (split) on the top surface so that the thickness of the tile varies slightly from one spot on the tile to another and from one tile to another.

  5. Marmorino - Wikipedia

    en.wikipedia.org/wiki/Marmorino

    Marmorino is made from crushed marble and lime putty, which can be tinted to give a wide range of colours. This can then be applied to make many textures, from polished marble to natural stone effects. Widely used in Italy, its appeal has spread through North America especially, but now worldwide. Because of the hours of workmanship, the ...

  6. Terrazzo - Wikipedia

    en.wikipedia.org/wiki/Terrazzo

    Terrazzo is a composite material, poured in place or precast, which is used for floor and wall treatments. It consists of chips of marble, quartz, granite, glass, or other suitable material, poured with a cementitious binder (for chemical binding), polymeric (for physical binding), or a combination of both. Metal strips often divide sections ...

  7. Marble - Wikipedia

    en.wikipedia.org/wiki/Marble

    Marble is a rock resulting from metamorphism of sedimentary carbonate rocks, most commonly limestone or dolomite. Metamorphism causes variable re-crystallization of the original carbonate mineral grains. The resulting marble rock is typically composed of an interlocking mosaic of carbonate crystals.

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