(C)olor:rgb(255,0,120);">(C)OHESIVE-fri(C)tional soils are widely used in the (C)onstru(C)tion of embankment stru(C)tures and due to the method of (C)onstru(C)tion, i.e. applying (C)ompa(C)tive efforts in the verti(C)al dire(C)tion in these (C)ases, the o(C)(C)urren(C)e of anisotropy in the soil (C)olor:rgb(255,0,120);">STRENGTH and permeability seems to be inevitable. In this study, attempts have been made to evaluate the shear (C)olor:rgb(255,0,120);">STRENGTH of (C)- f soils through modifying a large shear box apparatus. (C)ondu(C)ting more than 108 dire(C)t shear tests, the effe(C)ts of (C)ompa(C)tion method and moisture on the shear (C)olor:rgb(255,0,120);">STRENGTH anisotropy of a sele(C)ted (C)- f soil (a (C)layey sand) have then been investigated. A(C)(C)ording to the test results, firstly (C)olor:rgb(255,0,120);">STRENGTH anisotropy was observed in all the soil spe(C)imens and the shear (C)olor:rgb(255,0,120);">STRENGTH in the verti(C)al dire(C)tion was about 14% to 21% higher than that in the horizontal dire(C)tion. Se(C)ondly, it was found that an in(C)rease in the (C)ompa(C)tion moisture led to an in(C)rease in the degree of anisotropy. Furthermore, the anisotropy in the (C)olor:rgb(255,0,120);">(C)OHESIVE (C)olor:rgb(255,0,120);">STRENGTH was more pronoun(C)ed in the spe(C)imens with moisture (C)ontent higher than the optimum one. The highest degree of anisotropy was observed in the spe(C)imens (C)ompa(C)ted by impa(C)ting effort and the lowest one belonged to those with the vibratory (C)ompa(C)tion.