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Tehran is located in the Alborz's mountain range subsidence and alluvial deposits which are formed in the different faults. Though these faults caused changes in Northern Tehran's alluvium. The geomechanics factors on these alluviums made northern area of Tehran a dangerous place to construct. In this article we have tried to determine the zone's resistance , critical depth in excavation and in the end the role of faults in mechanical resistance of alluvium by comparing several pits in thedoi:10.4236/ojg.2017.78075 fatcat:tazbgmwerjh25nc42xkahf4fvm