A granular medium is viewed as a heterogeneous continuum that satisfies mec
hanical equilibrium at each material point. Analysis of the strain distribu
tion under deviatoric loading displays structures formation when the strain
pattern is filtered through a directionally sensitive deformation intensit
y analyzer. The same type of analysis carried out on numerical experiments
yields similar structures. Comparison between the two methods permits an es
timate of the radius of the mesodomain that is characteristic for granular
media. This scale is one of the necessary scales of discrimination that is
needed for the understanding of the deformation of granular materials with
elastofrictional particle interaction. Evolution of the thickness of the st
ructures is also analyzed. They become elongated with increasing deviatoric
deformation. The encroachment of the mesoscale onto the microscale (that i
s, the particle interactive scale) is signaled.