The present work deals with the theoretical investigation of the effect of Magnetic Field Dependent (MFD) viscosity of Soret-driven thermohaline convection of ferrofluid layer heated from below and salted from above saturating densely packed porous medium subject to a transverse uniform magnetic field. For a fluid layer contained between two free boundaries, an exact solution is obtained using a linear stability analysis. The normal mode method and Darcy model are used in the system. It has been observed that stationary mode is favorable for Darcy model. The critical magnetic thermal Rayleigh number NC for the onset of instability is also determined for sufficient large values of non-buoyancy magnetization parameter M1 and results are analyzed graphically. The MFD viscosity parameter is analyzed. The stabilizing behavior for various values of permeability of the porous medium, buoyancy magnetization parameter, ratio of mass transport to heat transport, thermal Rayleigh number and salinity Rayleigh number is studied. The salinity Rayleigh number has a destabilizing behavior for different values of non-buoyancy magnetization parameter, Soret parameter and MFD viscosity. It is also found that the MFD viscosity delays the onset of convection and MFD viscosity effect dominated the convective system.