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  2. Blackboard - Wikipedia

    en.wikipedia.org/wiki/Blackboard

    Stick-slip effect with a chalk on a blackboard. Chalk sticks are produced in white and in various colours, especially for use with blackboards. White chalk sticks are made mainly from calcium carbonate derived from mineral chalk or limestone, while coloured chalk sticks are made from calcium sulphate in its dihydrate form, CaSO 4 ·2H 2 O, derived from gypsum.

  3. Wholesaling - Wikipedia

    en.wikipedia.org/wiki/Wholesaling

    Wholesalers frequently physically assemble, sort, and grade goods in large lots, break-bulk, repack, and redistribute in smaller lots. [2] While wholesalers of most products usually operate from independent premises, wholesale marketing for foodstuffs can take place at specific wholesale markets where all traders are congregated .

  4. Michaels - Wikipedia

    en.wikipedia.org/wiki/Michaels

    Michaels Stores, Inc., more commonly known as Michaels, is a privately held retail chain of American and Canadian arts and crafts store. It is North America's largest provider of arts, crafts, framing, floral and wall décor, and merchandise for makers and do-it-yourself home decorators. [2]

  5. Federal Art Project - Wikipedia

    en.wikipedia.org/wiki/Federal_Art_Project

    The Federal Art Project (1935–1943) was a New Deal program to fund the visual arts in the United States. Under national director Holger Cahill, it was one of five Federal Project Number One projects sponsored by the Works Progress Administration (WPA), and the largest of the New Deal art projects.

  6. Chalkboard (disambiguation) - Wikipedia

    en.wikipedia.org/wiki/Chalkboard_(disambiguation)

    Chalkboard may also refer to: Chalkboard (typeface) See also. Blackboard (disambiguation) This page was last edited on 29 April 2022, at 23:48 (UTC). Text is ...

  7. Chalk - Wikipedia

    en.wikipedia.org/wiki/Chalk

    Chalk is a soft, white, porous, sedimentary carbonate rock.It is a form of limestone composed of the mineral calcite and originally formed deep under the sea by the compression of microscopic plankton that had settled to the sea floor.

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