A previously unknown form of charge ordering has been observed in dislocati
on free thin films of magnetite, Fe3O4. This charge ordering exists on tetr
ahedral sites and is unrelated to the well known low temperature ordering o
n octahedral sites that occurs below 120K. From modeling of electron diffra
ction patterns we deduce that the best fit to the observed diffraction patt
erns was obtained by reducing the scattering power on one tetrahedral site
per unit cell by about 80%.