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  2. Bedding - Wikipedia

    en.wikipedia.org/wiki/Bedding

    Some duvet or comforter sets do not include a top sheet; the duvet/comforter has a cotton bottom that replaces the sheet. Fitted sheet: This is the bottom sheet used to fit tightly over a mattress. Fitted sheets are available in a variety of pocket depths, which refers to the thickness of the mattress. Standard North American pocket size is 7 ...

  3. Bed sheet - Wikipedia

    en.wikipedia.org/wiki/Bed_sheet

    Bed sheets come in two main varieties: flat and fitted. A flat sheet is simply a rectangular sheet of cloth, while a fitted sheet has four corners, and sometimes two or four sides, fitted with elastic, to be used only as a bottom sheet. The fitted sheet may also be secured using a drawstring instead of elastic. The purpose of a fitted bottom ...

  4. Bed size - Wikipedia

    en.wikipedia.org/wiki/Bed_size

    In practice, bed sizes are usually categorized by the width. The length is typically 200 cm (79 in), but this may vary. The most common sizes are: [citation needed] 120 cm × 200 cm (47 in × 79 in) 150 cm × 200 cm (59 in × 79 in) 180 cm × 200 cm (71 in × 79 in) Other bed sizes are available, which are less common however.

  5. File:USMattressSizes.svg - Wikipedia

    en.wikipedia.org/wiki/File:USMattressSizes.svg

    Original file (SVG file, nominally 683 × 758 pixels, file size: 7 KB) This is a file from the Wikimedia Commons . Information from its description page there is shown below.

  6. Draw sheet - Wikipedia

    en.wikipedia.org/wiki/Draw_sheet

    A draw sheet is a small bed sheet placed crosswise over the middle of the bottom sheet of a mattress to cover the area between the person's upper back and thighs, often used by medical professionals to move patients. It can be made of plastic, rubber, or cotton, and is about half the size of a regular sheet.

  7. Graded bedding - Wikipedia

    en.wikipedia.org/wiki/Graded_bedding

    Graded bedding is a sorting of particles according to clast size and shape on a lithified horizontal plane. The term is an explanation as to how a geologic profile was formed. Stratification on a lateral plane is the physical result of active depositing of different size materials.

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