Page 300 - Introduction to Mineral Exploration
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12: CLIFFE HILL QUARRY AGGREGATE RESERVES  283



                        Railway line to Burton             Stud Farm          Stanton Lane  N      M1






                                        West Lane  Fig. 12.4      EXTN  Billa Barra Lane  Cliffe Hill

                 11                                                                       Quarry
                                                      Tythe Farm

                                       RWL                    NQ


                                                                          Stanton
                                                                       Street  Bardon  Processing
                                                                          under
                                                                                   Plant
                                                 Thornton Lane
                 10                                                  Main
                        0        500 m
                   44                   45                  46                  47                  48

                 FIG. 12.2  Cliffe Hill and Stud Farm Quarries, showing the location of some of the borehole sites (dots) and the
                 proposed new railway line (RWL). The pecked and dotted line represents the outline of the area included in
                 the planning permission. The pecked line represents the outline of the proposed new quarry (NQ) with the
                 possible extension shown to the east (EXTN).



                 land and mineral right holdings on Stud Farm.  tween the Triassic Mercia Mudstones and the
                 The study included a detailed literature search  markfieldite. The mudstones are also referred
                 which indicated that both Billa Barra Hill to  to as overburden which generally includes
                 the northwest, and Stud Farm around 1 km     glacial deposits as well.
                 to the west of the existing quarry might be of  The above exercises could be regarded as
                 potential interest (Fig. 12.1). The 1:63,360 and  separate phases or subphases, but since they
                 1:10,560 Geological Survey maps and the ac-  took place in swift succession they have been
                 count by Evans (1968) of the Precambrian rocks  regarded collectively as Phase 1. A cost (exclud-
                 of Charnwood Forest pointed to additional    ing overheads and geologist’s time) of around
                 areas of diorite near Stud Farm. A well sunk  £1500 was incurred for this work.
                 on Tythe Farm (Fig. 12.2) at the end of the last
                 century intersected markfieldite at a relatively
                 shallow depth.                               12.3  PHASE 2  – PRE- FEASIBILITY STUDY
                   Subsequent ground surveys eliminated the
                 former site as being composed of fine-grained  The preliminary desk study had indicated areas
                 tuff, volcanic breccia, and metasediments, but  of interest, but the Stud Farm holdings were
                 revealed scattered float boulders of mark-    insufficient to support a viable quarry (Bell &
                 fieldite in the soils at the latter site. In view of  Hopkins 1988). Negotiations were entered into
                 the total absence of exposures at Stud Farm, a  with the owner of adjacent land. An agreement
                 few pits were dug using a mechanical digger,  was reached which allowed Tarmac access
                 and although these failed to reach bedrock they  to the land for exploratory drilling. A small ex-
                 confirmed the existence of further pieces of  ploration drilling budget was approved and in
                 markfieldite in the soils. The term bedrock   mid 1978 nineteen, 150-mm continuous flight
                 in this chapter refers to the unconformity be-  auger holes were drilled with a Dando 250 top
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