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  1. Sundial, the earliest type of timekeeping device, which indicates the time of day by the position of the shadow of some object exposed to the suns rays. As the day progresses, the sun moves across the sky, causing the shadow of the object to move and indicating the passage of time.

    • Sundial

      Sundials are the oldest known instruments for telling time....

  2. en.wikipedia.org › wiki › SundialSundial - Wikipedia

    A sundial is a horological device that tells the time of day (referred to as civil time in modern usage) when direct sunlight shines by the apparent position of the Sun in the sky. In the narrowest sense of the word, it consists of a flat plate (the dial) and a gnomon, which casts a shadow onto the dial.

  3. A sundial is a device that measures time by the position of the Sun. In common designs such as the horizontal sundial, the Sun casts a shadow from the gnomon, which is a thin rod straight edge, onto a flat surface marked with lines indicating the hours of the day. The shadow cast by the end of the gnomon is the solar time at all times.

  4. All About Sundials. How Sundials Work. A detailed explanation of how the shadow of the sun allows you to tell the time, examples of different types of sundial, together with explanations of why sundials in different locations need to be at specific angles, the reasons why you have to adjust the ‘sun time’ to get “clock time”.

  5. pwg.gsfc.nasa.gov › stargaze › SundialThe Sundial - NASA

    The sundial is now ready, but you might use tape on the bottom of the base-sheet to hold the two pieces together firmly. For further stability, and to prevent the sundial from being blown away, you may attach its base with thumbtacks to a section of a wooden board or a piece of plywood. Finally, orient the fin to point north.

  6. A sundial is a device that indicates time by using a light spot or shadow cast by the position of the Sun on a reference scale. As the Earth turns on its polar axis , the sun appears to cross the sky from east to west, rising at sun-rise from beneath the horizon to a zenith at mid-day and falling again behind the horizon at sunset.