Earth's Day Changes Over Time
Tidal friction, driven mainly by the Moon, slows Earth’s rotation over the long term. The average secular effect is about 2.3 milliseconds added to the day per century, not 1.8 seconds. An approximately 21-hour day around 600 million years ago is based on geological evidence and models; the exact reconstruction is uncertain.
Synthetic illustration of Earth’s rotation and tidal braking.
