Noon cannot be everywhere at once
Why Is It a Different Day Somewhere Else?
Clocks are set by the Sun, and the Sun is only overhead in one place at a time.
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Step 1 of 5
A day is one turn of the Earth.
The Earth spins once in twenty-four hours, so every place passes under the Sun once. Noon is not a moment — it is a place.
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Step 2 of 5
Dividing the turn gives the zones.
Three hundred and sixty degrees divided by twenty-four hours is fifteen degrees an hour. Each stripe of fifteen degrees keeps one clock time.
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Step 3 of 5
Before railways, every town kept its own noon.
Clocks were set by the local Sun, so a town twenty miles east was minutes ahead. Timetables made that unworkable overnight.
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Step 4 of 5
The zones bend around countries.
The stripes are not straight. Borders pull them about so a country can share one time, and a few zones sit half an hour off the rest.
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Step 5 of 5
Somewhere the date has to change.
Go far enough east adding hours and you come back around. The line down the Pacific is where the arithmetic is forced to jump a whole day.
Two islands in the Pacific sit a few miles apart and twenty-five hours away from each other.
The short version
Time zones divide the Earth's twenty-four-hour turn into stripes, so clocks stay roughly in step with the Sun.
Try it yourself
Work out the time in a city eight zones away by adding eight hours. If it goes past midnight, it is tomorrow there.
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