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  2. Orbit of the Moon - Wikipedia

    en.wikipedia.org/wiki/Orbit_of_the_Moon

    Conversely, when the Moon reaches its apogee, its orbital motion is slower than its rotation, revealing eight degrees of longitude of its western (left) far side. This is referred to as optical libration in longitude. The Moon's axis of rotation is inclined by in total 6.7° relative to the normal to the plane of the ecliptic.

  3. Tidal locking - Wikipedia

    en.wikipedia.org/wiki/Tidal_locking

    In the case where a tidally locked body possesses synchronous rotation, the object takes just as long to rotate around its own axis as it does to revolve around its partner. For example, the same side of the Moon always faces Earth , although there is some variability because the Moon's orbit is not perfectly circular.

  4. Far side of the Moon - Wikipedia

    en.wikipedia.org/wiki/Far_side_of_the_moon

    A common misconception is that the Moon does not rotate on its axis. If that were so, the whole of the Moon would be visible to Earth over the course of its orbit. Instead, its rotation period matches its orbital period, meaning it turns around once for every orbit it makes: in Earth terms, it could be said that its day and its year have the ...

  5. Tidal acceleration - Wikipedia

    en.wikipedia.org/wiki/Tidal_acceleration

    The Moon pulls on each individual undulation as Earth rotates—some undulations are ahead of the Moon, others are behind it, whereas still others are on either side. The "bulges" that actually do exist for the Moon to pull on (and which pull on the Moon) are the net result of integrating the actual undulations over all the world's oceans.

  6. Near side of the Moon - Wikipedia

    en.wikipedia.org/wiki/Near_side_of_the_Moon

    The near side of the Moon is the lunar hemisphere that always faces towards Earth, opposite to the far side. Only one side of the Moon is visible from Earth because the Moon rotates on its axis at the same rate that the Moon orbits the Earth—a situation known as tidal locking.

  7. Moon - Wikipedia

    en.wikipedia.org/wiki/Moon

    The Moon is Earth's only natural satellite.It orbits at an average distance of 384,400 km (238,900 mi), about 30 times the diameter of Earth. Tidal forces between Earth and the Moon have synchronized the Moon's orbital period (lunar month) with its rotation period at 29.5 Earth days, causing the same side of the Moon to always face Earth.

  8. Why the moon shines so bright overhead in winter | The Sky Guy

    www.aol.com/why-moon-shines-bright-overhead...

    Did you ever wonder why the full moon seems so big and bright in the winter? Because the Earth’s axis is tilted about 23.5 degrees to its orbit around the sun, the sun appears at different ...

  9. Lunar precession - Wikipedia

    en.wikipedia.org/wiki/Lunar_precession

    Apsidal precession occurs when the direction of the major axis of the Moon's elliptic orbit rotates once every 8.85 years in the same direction as the Moon's rotation itself. This image looks upwards depicting Earth's geographic south pole and the elliptical shape of the Moon's orbit (which is vastly exaggerated from its almost circular shape ...