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the term fissure refers to a crack in a rock mass that is larger than the grain size of the rock. the term fracture refers to a crack in a rock mass that is smaller than the grain size of the rock. fissures and fractures are always associated with rock mass deformation, such as a rock fall.
the mechanically compacted subzone is the least resistant of all profiles. mechanical continuity of the fabric is less than in other subzones. this subzone may be subdivided according to the degree of compaction, the texture, and the nature of the parent material. generally, a mechanically compacted subzone is distinguished from a mechanically weak subzone by a greater degree of compaction and a greater degree of mechanical continuity of the fabric. in a mechanically weak subzone, no appreciable compaction has occurred and the texture is mechanically weak. in a mechanically compacted subzone, the texture is strong but the mechanical continuity of the fabric is weak. mechanical compacted subzones have low rupture resistance and are generally friable. if the soil material has appreciable shrink-swell potential, an internal crack appears if drying was sufficiently rapid. the most common occurrence is in soils that are well drained. the mechanically compacted subzone is shown in figure 3-7.
the mechanically weak subzone is subject to some compaction. in mechanically compacted subzones, it is usually not possible to distinguish a mechanically weak subzone from a mechanically compacted subzone. generally, a mechanically compacted subzone has a higher degree of mechanical continuity of the fabric and is less susceptible to cracking. in mechanically weak subzones, the texture is weak and the density is low. this subzone is often referred to as the subsoil. the mechanically weak subzone is shown in figure 3-8. 3d9ccd7d82
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