
The temperature at which a solid becomes a liquid at a given pressure.The melting point is the temperature at which a solid transitions to a liquid at a given pressure. At this temperature, the thermal vibrations of atoms or molecules overcome the interparticle forces that hold the solid lattice together, allowing the structure to break down into a disordered, flowing state. For pure substances, the melting point is a characteristic property, but it can be altered by pressure, impurities, or the presence of electric or magnetic fields.
The concept of a melting point has been known since antiquity, but it was quantified in the 18th century by scientists like Joseph Black, who distinguished between temperature and heat. The modern thermodynamic understanding was developed in the 19th century with the work of J. Willard Gibbs on phase equilibria.
In a solid, atoms are held in a regular lattice by attractive forces. As temperature rises, atoms vibrate more vigorously. At the melting point, the amplitude of these vibrations becomes large enough that the lattice structure becomes thermodynamically unstable, and the system transitions to a liquid phase where particles can move freely past one another. The melting point is determined by the balance between the enthalpy (heat content) and entropy (disorder) of the solid and liquid phases; at the melting point, the free energies of both phases are equal.
Melting points are used to identify substances, design alloys and materials with specific thermal properties, and in processes like 3D printing and casting, where controlled melting and solidification are essential.
The Mpemba effect, where hot water can freeze faster than cold water under certain conditions, is a counterintuitive phenomenon that challenges simple assumptions about cooling and freezing, and it is still not fully understood.













