In the present article the author continues to discuss the problem concerning identification of tectonic dislocations which can be seen on the surface as small relief forms, combined into lines, zones and fields which are clearly seen in satelitte photos as geometricized tonometric anomalies. A succession of morphotectonic dislocations is lined up with morphostructures at one end and criptomorphic formations on the other. The relationship between indication factors of criptomorphic formations and tectonic dislocations of different origin and age is also of a concern in the research.