Iron is the most abundant element in the Earth's core, especially in the liquid outer core (LOC), but also in the solid inner core, where other elements are present in significant concentration. Therefore Fe is very relevant in geophysics. The LOC stretches between ∼2,900 and 5,150 km depth, covers a pressure and temperature range from 135 to 330 GPa and from 4000 to 6500 K respectively, and comprises around 96% of the total core's volume. Consequently, the study of the properties of liquid iron (l-Fe) in such a high temperature and pressure regime is a topic of geophysical interest. The understanding of important phenomena that occur in the core, such as the generation of the magnetic field, and the heat and mass transport, requires a good knowledge of the dynamic properties of l-Fe.Without intending to be exhaustive of the wealth of research already performed about l-Fe, we make below a short review of those aspects that have been studied and are related to our present work. We will mention experimental measurements and theoretical calculations, based on Molecular dynamics (MD) simulations, that have addressed thermodynamic, structural and transport properties of l-Fe.