We present a theory of the melting of elements as a dislocation-mediated ph
ase transition. We model dislocations near the melt as noninteracting close
d loops on a lattice. In this framework we derive simple expressions for th
e melting temperature and latent heat of fusion that depend on the dislocat
ion density at melt. We use experimental data for more than half the elemen
ts in the periodic table to determine the dislocation density from both rel
ations. Melting temperatures yield a dislocation density of (0.61+/-0.20)b(
-2), in good agreement with the density obtained from latent heats, (0.66+/
-0.11)b(-2), where b is the length of the smallest perfect-dislocation Burg
ers vector. Melting corresponds to the situation where, on average, half of
the atoms are within a dislocation core.