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DISCONTINUOUS SUBSIDENCE ASSOCIATED WITH CAVING METHODS OF MINING



















              Figure 16.10  Schematic representa-
              tion of the surface subsidence result-
              ing from block caving, and associated
              definitions.

                                        inclined surface slopes forming only in weak or weathered surface layers. However, a
                                        number of features of the orebody and the local geology and topography can influence
                                        the extent of the surface expression of caving. These factors include (Brown, 2003):
                                           the dip of the orebody;

                                           the shape of the orebody in plan;

                                           the strength of the orebody;

                                           the strength of the surrounding country rock;

                                           the strength of the overburden or cap rock;

                                           the presence of major structural features such as faults and dykes intersecting the

                                           orebody and cap rock;
                                           the depth of mining as defined by the undercut level and the associated in situ

                                           stress field;

















              Figure 16.11  Plan view of the sub-
              sidence crater at the El Teniente Mine,
              Chile, in 1998 showing the Braden
              Pipe and the locations of several
              production sectors (after Karzulovic
              et al., 1999).
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