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Interpretation of satellite images is one of the methods used in geological studies. Accessibility and the relatively small cost of images has led to remote-sensing methods becoming one of the basic tools for analysing and displaying: the identifi cation of rocks and soils, geological structures, mineral resources, oil, geothermal waters, the monitoring of geological phenomena and the identifi cation of the form of the terrain. After several decades of use, the consensus among experts is that the basic benefi t of using remote-sensing materials services in geology is the possibility to obtain information with regard to tectonics [1, 7, 11]. Robert Helbling is the founding-father of photogeology and in the 1930s, in the Alpine massif, he conducted studies concerning cartography and geology, photointerpretation and photogrammetric. These studies can be applied to larger areas through the use of the same methods and research parameters and enable the use of greater accuracy as well as cost reduction and the acceleration of studies [5]. It has been confi rmed by current geological studies [11, 25]. The advantage of graphic material is strict dating and the possibility of repeated studies by means of various criteria and methods. It also allows for easy repetition of studies at diff erent times, as well as the monitoring of changes. The possibility of the complementary use of the photogeology is particularly important, through the use of modern methods of aerial and satellite geophysics, the observation of magnetic and radiometric images, cartographic references, the digital terrain model and the implementation of further geological works in selected regions without the examination of the entire area [4, 11, 22]. The main factor for the surface of the area which may be noted using remote-sensing methods is lineaments. This ambiguous term was introduced to the geological literature at the beginning of the 1930s by Hobbs, though it was examined

geomatics and environmental engineering

Determination of geological linear structures of the Low Beskids – assessment of suitability of Landsat 8 satellite images and products of the image processing.