 The stratified sequence that can be seen today is the result of sedimentation that was interrupted by erosional processes like deflation.That sequence, based on the small-scale animal disturbance in a thin section of the strata, was most likely stable for millions of years.According to Macphail and McAvoy's analysis, it appears that the site is intact with only a few minor disturbances that could affect the long-term integrity of the site's stratigraphy.