Anisotropic characteristics of granular soil, consolidated to various initial stress states, were evaluated under generalized strain paths using hollow cylinder torsional shear tests. Fraser River sand samples prepared by water pluviation were subjected to isotropic and anisotropic consolidation stresses and sheared under undrained conditions along specific strain paths characterized by constant intermediate principal strain parameter (๐ ๐ ) and various fixed principal strain directions (๐ผ ๐ ). A series of tests along different inclinations of the major principal strain with respect to the vertical depositional direction permitted an assessment of the interaction between principal strain directions and fabric. A decrease in strain hardening tendency is observed as the major principal strain aligned towards the bedding plane. Considering different levels of anisotropic consolidation stresses also allowed a detailed examination of how initial static shear affects the responses. In particular, generated principal stresses and their direction, as well as the pore pressure responses, were closely examined. Novel findings, that highlight range of intermediate principal stress parameter (๐ ๐ ) associated with the undrained plane strain condition, and the interaction between ๐ ๐ and ๐ ๐ during shearing are presented. It was found that ๐ ๐ systematically decreases with shear strain in constant ๐ ๐ tests. The ๐ ๐ value in plane strain tests (๐ ๐ =0.5) was found to be in the range of 0.2 to 0.4 depending on the loading path, and the stage of shearing.The relationship between principal stress directions and plastic-strain increment directions was assessed to identify the nature of plasticity in the material. In order to ensure confident assessment of non-coaxiality, total strain was decomposed into elastic and plastic strain. The existence of non-coaxiality in Fraser River sand (FRS) was observed when the sand was subjected to undrained shear at fixed principal strain directions that do not coincide with the fabric axis of symmetry. Non-coaxiality was not observed when the principal directions of stress/strain coincided with the fabric axis of symmetry. It was also noticed that irrespective of the initial condition, the degree I would also like to express my special and sincere thanks to my second supervisor Dr. Mehdi Pouragha, who joined me in the second half of my journey, and provided me with continuous guidance, essential support and valuable suggestions at every phase of the analytical part of the research. In particular, encouraging and guiding me to use Matlab and Latex was one of the great things that saved me a lot of time. This thesis would not have been possible without his constant assistance and endless patience.I would like to thank Dr. Gertraud Medicus, Dr. Sai Vanapalli, Dr. Mohammad Rayhani, and Dr. Elena Zabolotnii, for being members in my examination committee and for providing valuable suggestions. I further thank Dr. Gertraud Medicus for the open-source MATLAB code for M-N surface uploaded on SoilModels....