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The basin of diapir anticlinal from Ocna Şugatag entered into the accelerated transformation soon after the cessation of exploitations (the beginning of the years '60). Along of the most 50 years of evolution formed and disappeared lacustrine basins, all on natural way in little dolines, mostly all of them, through the breakdown of galleries or halls of salt exploitation, with the individualization of greatest lacustrine basins. These dynamics rearward are very accelerated, the evidence beeingdoaj:6c02a94dde8941aa846a282550f6d692 fatcat:dwmxgfv47nfbtoiy6cnqn5fafq