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  2. Procedural texture - Wikipedia

    en.wikipedia.org/wiki/Procedural_texture

    These kinds of textures are often used to model surface or volumetric representations of natural elements such as wood, marble, granite, metal, stone, and others. Usually, the natural look of the rendered result is achieved by the usage of fractal noise and turbulence functions [ definition needed ] .

  3. List of types of marble - Wikipedia

    en.wikipedia.org/wiki/List_of_types_of_marble

    Marble mis-nomers: Cetechovice marble (cetechovický mramor) from Cetechovice, Kroměříž District: coloured [c] Karlík marble (karlický mramor), from Barrandien, Karlík, Prague-West District: black with gold-yellow-colour veins [d] Podol marble (Podolský mramor), from Vápenný Podol, Chrudim District: white, grey-white, rosy [e]

  4. Faux painting - Wikipedia

    en.wikipedia.org/wiki/Faux_painting

    Marbleizing or faux marbling is used to make walls and furniture look like real marble. This can be done using either plaster or glaze techniques. Fresco is a simple technique, uses mixtures of tint and joint compound to add mottled color and subtle texture to plain walls,

  5. List of art media - Wikipedia

    en.wikipedia.org/wiki/List_of_art_media

    Media, or mediums, are the core types of material (or related other tools) used by an artist, composer, designer, etc. to create a work of art. [1] For example, a visual artist may broadly use the media of painting or sculpting, which themselves have more specific media within them, such as watercolor paints or marble.

  6. The Blue Marble - Wikipedia

    en.wikipedia.org/wiki/The_Blue_Marble

    The Blue Marble is a photograph of Earth taken on December 7, 1972, by either Ron Evans or Harrison Schmitt aboard the Apollo 17 spacecraft on its way to the Moon.Viewed from around 29,400 km (18,300 mi) from Earth's surface, [1] a cropped and rotated version has become one of the most reproduced images in history.

  7. Marble - Wikipedia

    en.wikipedia.org/wiki/Marble

    Marble is a metamorphic rock consisting of carbonate minerals (most commonly calcite (CaCO 3) or dolomite (CaMg(CO 3) 2) that have recrystallized under the influence of heat and pressure. [1] It has a crystalline texture, and is typically not foliated , although there are exceptions.