Using adiabatic hydrodynamical simulations, we follow the evolution of two symmetric cold fronts developing in the remnant of a violent z=0.3 massive cluster merger. The structure and location of the simulated cold fronts are very similar to those recently found in X-ray cluster observations, supporting the merger hypothesis for the origin of at least some of the cold fronts. The cold fronts are preceded by an almost spherical bow shock which originates at the core and disappears after 1.6 Gyr. The cold fronts last longer and survive until z=0. We trace back the gas mass constituting the fronts and find it initially associated with the two dense cores of the merging clusters. Conversely, we follow how the energy of the gas of the initial merging cores evolves until z=0 from the merging and show that a fraction of this gas can escape from the local potential well of the sub-clumps. This release occurs as the sub-clumps reach their apocentre in an eccentric orbit and is due to decoupling between the dark matter and part of the gas in the sub-clump because of, first, heating of the gas at first close core passage and of, second, the effect of the global cluster pressure which peaks as the centrifugal acceleration of the sub-clump is maximal. The fraction of the gas of the sub-clump liberated in the outbound direction then cools as it expands adiabatically and constitutes the cold fronts.
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