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Time and Calendars · entry 24 of 52
A sundial's shadow points roughly north at local noon in the Northern Hemisphere.
The longer version
For observers in most of the Northern Hemisphere, the Sun stands due south at local noon, so any shadow falls toward the north. A dial set up correctly will therefore show its shortest shadow of the day pointing along the north-south line. The shadow is also at its shortest then, since the Sun is highest.
That moment is not what a clock reads at twelve, because time zones average solar time over a wide band and daylight saving adds another hour. The gap between sundial noon and clock noon can be substantial, which surprises people who assume the two should agree. Longitude within the zone explains most of the difference.
Where this entry sits
These facts wander through clocks, calendars, time zones, and the long human effort to measure passing hours. You will find leap years, odd month lengths, ancient sundials, and the reasons modern timekeeping works the way it does. The full list sits on the Time and Calendars page, where every entry is listed in order.
More From Time and Calendars
Eight more entriesHourglasses measure time by letting fine sand fall through a narrow opening at a steady rate.
Read 26Water clocks were among the earliest timekeepers, using a steady drip to mark passing hours.
Read 27Candle clocks marked time by burning evenly, with markings showing how much had melted.
Read 28The pendulum clock improved accuracy by using a swinging weight to regulate each tick.
Read 29Pendulums swing at a rate determined mostly by their length rather than by their weight.
Read 30Quartz clocks keep time by counting the vibrations of an electrically stimulated quartz crystal.
Read 31Atomic clocks measure time by counting the natural vibrations of atoms, making them extraordinarily precise.
Read 32Navigation satellites depend on extremely accurate onboard clocks to calculate positions on Earth's surface.
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