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Back before Astronomy was well-understood, people used the "Apparent" motion of the Sun across the sky as the measure of the length of the day. Now that we know better, we measure the length of a day as one complete rotation of the Earth. This is known as a sidereal day (sigh-deer-ee-al) which is approximately 23 hours, 56 minutes, 4.09 seconds, corresponding to the time it takes for the Earth to complete one rotation with reference to the vernal equinox.

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