In the master's thesis, we scanned the Mlačca ice climbing wall in three term measurements with a Leica BLK360 terrestrial laser scanner and a Leica Nova MS60 image tachymeter. We were interested in the thickness of the ice according to the term measurement. For georeferencing point clouds, we stabilized a network of targets on the opposite side of the ice climbing wall. We determined the spatial coordinates of the network of targets in the manner of classical terrestrial geodetic measurement. Using the static GNSS measurement method, we provided the geodetic datum in the national coordinate system D96-17/TM(ESRS). After the measurements, we performed an analysis of the wall thickness according to the term measurement and the type of instrument used. We presented the results graphically and created cross sections of the ice climbing wall for three imaginary climbing directions. The thickness of the ice was shown numerically on the cross sections. We found that when scanning ice, the angle of incidence of the laser beam and the wavelength of the instrument had a great influence on the quality of the data. The amount of water on the surface of the ice is also important, as it greatly affects the reflectivity of the laser beam.
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