Due to the Universal law of gravitation, we know that objects of equal mass have a larger gravitation force between them when they are closer together. Because the near side of the Earth is closer to the Moon than the far side of the Earth, the force between the Moon and the near side of Earth is greater than the force between the Moon and the far side of Earth. This difference in forces causes the Earth to stretch along the Earth-Moon line, which causes a bulge on the near side of the Earth and a bulge on the far side of the Earth. This stretching is caused by a “tidal force” and causes the rising and falling of tides on Earth as the Moon continues its orbit.
George Darwin, Charles Darwin’s son, was the first to mathematically illustrate the theory of tidal friction. Tidal friction occurs because, as the Moon continues along its orbit, the Moon’s gravity attempts to pull the bulges right along with it, while the Earth attempts to pull the bulges along with it as it rotates. A torque is produced and a friction between Earth and the tides slows down the rotation of the Earth. Due to the conservation of angular momentum, the Earth’s loss of angular momentum becomes the Moon’s gain of angular momentum1.
This transfer of angular momentum results in the slowing of Earth’s rotation and the growing of the Moon’s orbit. These changes occur very slowly; the length of a day increases by about 1 second every 50,000 years1. However, these seconds add up and it is likely that early Earth had a day of only about five or six hours and the Moon was far closer to the Earth than it is now1. Tidal friction also explains the synchronous rotation of the Moon; as the tidal force from the Earth slowed the Moon down, it eventually rotated at the same rate as its bulges1. Eventually, the Earth could have a synchronous rotation toward the Moon and have days as long as its months. However, this likely would not last consistently due to the tidal forces of the Sun.
[1] Bennett, Jeffery, et al. The Cosmic Perspective: The Solar System. 9th ed., Pearson, 2020.










