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  2. Shelf (storage) - Wikipedia

    en.wikipedia.org/wiki/Shelf_(storage)

    Shelf (storage) A shelf ( pl.: shelves) [1] is a flat, horizontal plane used for items that are displayed or stored in a home, business, store, or elsewhere. It is raised off the floor and often anchored to a wall, supported on its shorter length sides by brackets, or otherwise anchored to cabinetry by brackets, dowels, screws, or nails.

  3. 40 Reading Nooks We Actually Want to Curl Up In - AOL

    www.aol.com/35-reading-nooks-inspire-inner...

    Create Custom Built-Ins. ... Take note of this space designed by Shapeless Studio and install wall-to-wall floating shelves for a linear, clean display. Give the space a new twist and bonus ...

  4. Floating shelf - Wikipedia

    en.wikipedia.org/wiki/Floating_shelf

    A floating shelf can be supported on hidden rods or bars that have been attached to studs. A thick floating shelf may be made of a hollow-core shelf glued to a cleat. [6] A floating shelf may have two or more channels open from the back towards, but without reaching, the front, into which slide fasteners attached to the wall, typically held in ...

  5. The best websites to buy discount furniture and home ... - AOL

    www.aol.com/lifestyle/best-websites-affordable...

    If you’re looking for something specific, from floating nightstands to custom shelving, Etsy is a great first stop. It’s also a perfect place to look for vintage and secondhand furniture and ...

  6. Shelf ice - Wikipedia

    en.wikipedia.org/wiki/Shelf_ice

    Structure. Shelf ice is a floating mat of ice, but unlike a pond or a small lake that freezes over, the shelf is not a uniform sheet of ice. Created by the wind and waves, the shelf ice is a jumble of ice chunks, pushed onto each other. It is as if you took a pile of rubble and pushed up against a wall.

  7. Ice shelf - Wikipedia

    en.wikipedia.org/wiki/Ice_shelf

    An ice shelf is "a floating slab of ice originating from land of considerable thickness extending from the coast (usually of great horizontal extent with a very gently sloping surface), resulting from the flow of ice sheets, initially formed by the accumulation of snow, and often filling embayments in the coastline of an ice sheet." [5] : 2234.

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