Introduction. The Kungur Ice Cave’s complex morphology indicates several stages of formation, starting with hypogenic (phreatic), and then epigenic (vadose) stages of speleogenesis. Cave formation conditions determined its specific water content and unique morphometry. Research objective was to create an actual topographic plan of the cave to establish morphometric parameters of the underground cavity (length, average width and height of the grottoes, amplitude, area and volume, etc.). Methods of research consisted in the graphical interpretation of the data obtained during topographic surveys performed by modern geodetic instruments and an alternative method of surveying underground cavities using a modified laser rangefinder. The surveys were carried out in the cave in the period from 2018 to 2021. Research results. For the first time, the volumes of individual grottoes and passages were calculated for the cave. In the protected part of the cave, the levels of lakes, the sole and roof of galleries were tied to absolute heights. The area occupied by the mantle ice in the cave was determined. The areas of lakes during the period of minimum and maximum water levels are calculated, as well as the strength of rocks over the entire cave. The area occupied by the mantle ice at the beginning of 2022 was determined. Within the framework of structural mapping, genetic types of cracks were recorded (tectonic, intrastratal, separation, hydration and tension, dissolution cracks), their total length was more than 38 km. We obtained marks of clay-dolomite interlayers separated in the ice-cave pack and marks of the stable water level at the time of the cave formation (10–12 thousand years ago). For the first time, the sole of the Nevolinskaya sequence was mapped in absolute hights, the area and number of organ pipes were revealed, and the zone of areal development of sulfate and carbonate breccia was identified. The scope of the results. The analysis of the obtained structural mapping data will allow us to assess the stability of the walls and the vaulted part of the grottoes, which will further increase the safety of visiting the excursion part of the cave.
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