The Mohr-Coulomb theory is a critical model for understanding the plasticity of materials like soil and rock, incorporating both frictional and dilatational effects. It addresses limitations of standard J2 - von Mises yield criteria, which often fail to account for pressure sensitivity in plastic deformation. The yield condition in Mohr-Coulomb theory states that yielding occurs when a specific combination of shear stress and mean normal stress is reached, defined by the equation τ = c - μσ. This model is visualized as a wedge-shaped yield surface, reflecting the angle of internal friction and its dependency on mean normal stress. The Drucker-Prager model is noted as a more effective alternative in numerical applications due to its improved behavior.