Fig. 2: Detailed revision of the geological map of the Fushe-Verri region resalted in making out one prospect, which locates in the southern continuation of the eroded anticline of Kalasa. The prospect does not locate coaxial to the eroded anticline, as it shifts southward in form of humankind step. Q Quaternary, Pg₃² Middle Oligocene, Pg₃¹ Lower Oligocene, Pg₃¹ tp Transitional marl package, Pg₁₊ Pg₂ Paleocene and Eocene, T_{3 e, d} Upper Triassic evaporitic and dolomitic deposits.