Glasses are
amorphous solids, which are usually fabricated when the molten material cools very rapidly to below its glass transition temperature, without sufficient time for a regular crystal lattice to form. Solids are characterised by a high degree of connectivity between their molecules, and fluids have lower connectivity of their structural blocks. Melting of a solid material can also be considered as a percolation via broken connections between particles e.g. connecting bonds. In this approach melting of an amorphous material occurs, when the broken bonds form a percolation cluster with
Tg dependent on quasi-equilibrium thermodynamic parameters of bonds e.g. on enthalpy (
Hd) and entropy (
Sd) of formation of bonds in a given system at given conditions: :T_g = \frac{H_d}{S_d+ R \ln(\frac{1-f_c}{f_c})}, where
fc is the percolation threshold and
R is the universal gas constant. Although
Hd and
Sd are not true equilibrium thermodynamic parameters and can depend on the cooling rate of a melt, they can be found from available experimental data on
viscosity of amorphous materials. Even below its melting point, quasi-liquid films can be observed on crystalline surfaces. The thickness of the film is temperature-dependent. This effect is common for all crystalline materials. This
pre-melting shows its effects in e.g. frost heave, the growth of snowflakes, and, taking grain boundary interfaces into account, maybe even in the movement of
glaciers. ==Related concept==