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  2. 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 ...

  3. Wooden 7 Cube Book Shelf. If you're on the hunt for a simple wood option that'll match the mid-century modern vibe of your humble abode, this top-rated style fits the bill.

  4. 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.

  5. Antarctic ice sheet - Wikipedia

    en.wikipedia.org/wiki/Antarctic_ice_sheet

    The Antarctic ice sheet is a continental glacier covering 98% of the Antarctic continent, with an area of 14 million square kilometres (5.4 million square miles) and an average thickness of over 2 kilometres (1.2 mi). It is the largest of Earth's two current ice sheets, containing 26.5 million cubic kilometres (6,400,000 cubic miles) of ice ...

  6. 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.

  7. Ice calving - Wikipedia

    en.wikipedia.org/wiki/Ice_calving

    Ice calving, also known as glacier calving or iceberg calving, is the breaking of ice chunks from the edge of a glacier. [1] It is a form of ice ablation or ice disruption. It is the sudden release and breaking away of a mass of ice from a glacier, iceberg, ice front, ice shelf, or crevasse. The ice that breaks away can be classified as an ...

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