A state where one side of a planet always faces its star.Tidal locking is a gravitational phenomenon in which a celestial body, such as a planet or moon, always shows the same face to the object it orbits. This happens because the gravitational pull from the larger body creates a tidal bulge on the smaller one, and over time, the smaller body's rotation slows until its rotational period matches its orbital period. The most familiar example is the Moon, which is tidally locked to Earth, which is why we only ever see one side of it.
The concept was first mathematically described by George Darwin (son of Charles Darwin) in the late 19th century, who studied the tidal evolution of the Earth-Moon system.
The gravity of the central body (like a star) stretches the orbiting body into a slight ellipsoid, creating a tidal bulge. If the orbiting body rotates faster than it orbits, the bulge is carried ahead of the line connecting the two bodies. The central body's gravity then pulls back on this offset bulge, exerting a torque that slows the rotation. Over millions of years, this torque gradually synchronizes the rotation with the orbital motion, locking one hemisphere to face the central body.
Tidal locking is a key consideration in exoplanet research, as planets in the habitable zone of red dwarf stars are often tidally locked, affecting their climate and potential habitability.
Mercury is not tidally locked to the Sun in a simple 1:1 resonance, but rather in a 3:2 spin-orbit resonance, meaning it rotates three times for every two orbits.






