The exploitation of the gem salt from the Targu Ocna Salt Mine, Trotuș Mine, Romania, due to the mining voids created, the initial stability of the massif was destroyed, the hydrogeological conditions of the deposit were gradually modified. The sterile intercalations, especially clayey, which acted as a protective shield against water infiltration, being cracked or broken, opened the possibility of water infiltration through the stratification planes, faults, fissures and cracks. The water coming from the condensation on the ceiling, walls and hearth of the mining works produced superficial dissolution phenomena. After drying, the solidified salt remained on the surfaces of the ceiling, walls or hearth of the excavated spaces. The most illustrative area in this regard is the entrance from the car plan to the V horizon of the Trotus Mine, where the hearth and the ceiling of the rooms are covered with recrystallized salt. On 17.10.2024, when a visit was made underground, before the entrance gate and then approx. 100 meters, at the hearth of the room there were numerous puddles, with a depth of 5-10 cm. The presence of water in the salt massif generated dissolution phenomena, which affected the bearing capacity of the resistance elements, pillars and floors, in two ways, namely the reduction of the values of the mechanical resistances over time and the reduction of the dimensions of the resistance elements, due to the dissolutions. The limitation of the phenomena of infiltration of water into the groundwater can be achieved, in the first instance, by carrying out, on the surface, some water capture and drainage works, apart from the cones of collapse of the old basins. In this regard, guard channels, gutters, ditches, or regularization works of the riverbeds of the Trifu and Grebleş streams that cross the exploitation perimeter can be built. In order to monitor the stability of the land surface in the salt mining perimeter, in addition to the topographic landmarks, located on the area adjacent to the perimeter, continuous monitoring of the morphology of the land was introduced, through aerial photogrammetry from drones. This method allows the construction of continuous, high-precision three-dimensional digital models of the land surface of the entire mining perimeter.