A configuration of matter in the Earth based on describable inhomogeneity, pattern, or fracture in an EarthMaterial. 
The identity of a GeologicStructure is independent of the material that is the substrate for the structure. 
Properties like "clast-supported",  "matrix-supported", and "graded bed" that do not involve orientation are considered kinds of GeologicStructure 
because they depend on the configuration of parts of a rock body. Includes sedimentary structures.
The general GeologicRelation is used to associate penetrative GeologicStructures with GeologicUnits.
    
 
    
    
        
                
                    
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