Abstract: Tertiary rocks of Changkikong Range constitutes a part of belt of Schuppen- a most prominent morphotectonic unit of Naga Hills. The palaeocurrent patterns for the Barail Group (Tikak Parbat Formation) , Changki Formation and Tipam Group (Tipam Sandstone Formation) have been studied . Interpretation reveals polymodal, bimodal , bimodal-pipolar palaeocurrent patterns in the study area.