摘要：Risks concerning the evolution of mesothermic stratification on the salt lakes from Sovata. Speed of scroll of the phenomena and the process in the space of the anticlinal basin from Sovata, associate to the anthropic intervention, influence the lacustrine dynamics, inclusively the natural specific outpourings, how he is the heliotherm phenomenon. The different mobility of the versants, the amplitude of the process of dissolution of the salt, the relative erect values of the watery transit through the system of lakes, the intense activity concerning the bathes, the different development of forest vegetation around lacustrine units etc., they fill the substantial modifications in the thermic stratification on specific vertical the salt lakes, carry can come up to the disappearance of the heliotherm phenomenon. The taking of protective specific measures: the versants consolidation in contiguously of the lakes, the brooks catchment before their lacustrine system transit and their deviation to the system of sewerage of the resort, the drain of underground waters from zone, the complet arrangement of the lacustrine basins and the bath restraint, the ablution of the shafts on a band of outline of at least five meters etc., they can contribute significantly to the thermic stratification normalization and to the mezoterm horizon preservation, wich contribute significantly to the development of the resort from Sovata
