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Based on the field observation results of ground pressure in shallow seam, the movement characteristics of overlying strata in front and behind and the subsidence of the earth’s surface are studied. Also, the paper analyzes the stability of overlying bedrock according to the theory of voussoir beam’s “S-R” stability and the hypothesis of step subsidence. It points out that slide instability is the fundamental form of overlying bedrock movement.
Based on the field observation results of ground pressure in shallow seam, the movement characteristics of overlying strata in front and behind and the subsidence of the earth’s surface are studied. Also, the paper analyzes the stability of overlying bed rr according to the theory of voussoir beam’s “SR ” stability and the hypothesis of step subsidence. It points out that slide instability is the fundamental form of overlying bedrock movement.