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  2. Sandpainting - Wikipedia

    en.wikipedia.org/wiki/Sandpainting

    Navajo sandpainting, photogravure by Edward S. Curtis, 1907, Library of Congress. In the sandpainting of southwestern Native Americans (the most famous of which are the Navajo [known as the Diné]), the Medicine Man (or Hatałii) paints loosely upon the ground of a hogan, where the ceremony takes place, or on a buckskin or cloth tarpaulin, by letting the coloured sands flow through his fingers ...

  3. Sands of the Nile - Wikipedia

    en.wikipedia.org/wiki/Sands_of_the_Nile

    Stirring the water with his hand, the water turns murky or black. The colored sands are then poured into the bowl and stirred by hand. With a flourish, the magician reaches into the bowl to pull out each color of sand, separate and unmixed. With a last stir, the water turns clear again, with a few stray grains of sand left in it.

  4. Seven Coloured Earths - Wikipedia

    en.wikipedia.org/wiki/Seven_Coloured_Earths

    The Seven Coloured Earths are a geological formation and prominent tourist attraction found in the Chamarel plain of the Rivière Noire District in south-western Mauritius.It is a relatively small area of sand dunes comprising sand of seven distinct colours (approximately red, brown, violet, green, blue, purple and yellow).

  5. Sand mandala - Wikipedia

    en.wikipedia.org/wiki/Sand_mandala

    Many sand mandala contain a specific outer locality which is clearly identified as a charnel ground. The colors for the painting are usually made with naturally colored sand, crushed gypsum (white), yellow ocher, red sandstone, charcoal, and a mixture of charcoal and gypsum (blue). Mixing red and black can make brown, red and white make pink.

  6. Alum Bay - Wikipedia

    en.wikipedia.org/wiki/Alum_Bay

    The cliffs of Alum Bay, showing the steeply-dipping multi-coloured sands above the white Chalk, with shallower dips towards the northern end. Alum Bay is the location of a classic sequence of upper Paleocene and Eocene beds of soft sands and clays, separated by an unconformity from the underlying Cretaceous Chalk Formation that forms the adjoining headland of West High Down.

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