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Technical and Strategic Assessment of Aggregate Supply Options in ...

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<strong>Technical</strong> & <strong>Strategic</strong> <strong>Assessment</strong> <strong>of</strong> <strong>Aggregate</strong> <strong>Supply</strong> <strong>Options</strong> <strong>in</strong> the South West Region<strong>and</strong>, <strong>in</strong> the case <strong>of</strong> quarries that are actively work<strong>in</strong>g below the water table, they couldpotentially restrict current <strong>and</strong> future rates <strong>of</strong> production. These effects should be m<strong>in</strong>imalfor most quarries (not least because <strong>of</strong> the entitlement to compensation for any asset valuelost before 2012) but the impact could potentially be very serious <strong>in</strong> areas (such as theMendips) where major aggregate quarries requir<strong>in</strong>g large scale dewater<strong>in</strong>g exist with<strong>in</strong>groundwater catchments that are extensively used for public water supply. The preciseimplications <strong>of</strong> this cannot be assessed until more is known about the way <strong>in</strong> which the newlicences will be determ<strong>in</strong>ed, although a number <strong>of</strong> scenarios could usefully be developed toillustrate some <strong>of</strong> the potential consequences. This, however, would require site-specific<strong>in</strong>formation on the proportions <strong>of</strong> reserves above <strong>and</strong> below the natural water table, <strong>and</strong>above <strong>and</strong> below the current (drawn-down) water table. Such <strong>in</strong>formation is not currentlyavailable.Table 4.1: Permitted Reserves <strong>and</strong> Annual Output (<strong>in</strong> 2001) for Groups <strong>of</strong> L<strong>and</strong>-Based Primary <strong>Aggregate</strong> Sources <strong>in</strong> South West Engl<strong>and</strong>Groups <strong>of</strong> Sources 2001 Reserves 2001 Output2001Output LifeSub-Totals(see Appendix A for details <strong>of</strong> each group, <strong>and</strong> Figures 4.1 to 4.3 for locations) (Mt) (Mt) (Mt) (yrs)HARD ROCK AGGREGATE SOURCES: 0 0 0 0A: Carboniferous Limestone, Mendips, Somerset 638.75 13.03 49B: Carboniferous & Devonian Limestone, Somerset & Devon 124.96 2.18 57C: Carboniferous Limestone, North Somerset 61.00 2.45 25D: Carboniferous Limestone, Gloucestershire (Forest <strong>of</strong> Dean) 16.90 1.43 12E: Carboniferous Limestone, South Gloucestershire 183.00 3.02 6125.41F: Granite & Gabbro, SW Cornwall 124.03 0.93 133G: Granite, N Cornwall & Dartmoor 50.74 0.48 105H: Dolerite, Devon & Cornwall, plus Andesite, Somerset 87.79 1.24 71I: Carboniferous <strong>and</strong> Devonian S<strong>and</strong>stone, Devon & Cornwall 21.20 0.59 36J: Carboniferous & Devonian S<strong>and</strong>stone, Somerset <strong>and</strong> South Gloucestershire 3.60 0.0661‘WEAK’ ROCK AGGREGATE SOURCES: 0 0 0 0K: Jurassic Portl<strong>and</strong> Limestone, Dorset 46.32 0.39 119L: Jurassic Limestone & Cretaceous Chalk, exclud<strong>in</strong>g Groups K <strong>and</strong> M 2.10 0.07 1.2032M: Jurassic Limestone, Gloucestershire 14.37 0.7419LAND-BASED SAND & GRAVEL AGGREGATE SOURCES: 0 0 0 0N: Permian & Triassic S<strong>and</strong> & Gravel, Devon 12.05 1.02 12O: Cretaceous to Quaternary S<strong>and</strong> & Gravel, Devon & Cornwall 3.05 0.19 16P: Cretaceous to Quaternary S<strong>and</strong> & Gravel, Wiltshire 11.66 1.39 5.258Q: Quaternary <strong>and</strong> Triassic S<strong>and</strong> & Gravel, Gloucestershire 11.77 0.88 13R: Tertiary & Quaternary S<strong>and</strong> & Gravel, Dorset 26.89 1.77Totals (Mt) 1440.17 31.86 4515SOURCE: SWRAWP, February 20054.9 The <strong>in</strong>creased breakdown shown <strong>in</strong> Table 4.1, compared with that given <strong>in</strong> the SWRAWPannual report, 2001, allows a more detailed exam<strong>in</strong>ation to be made <strong>of</strong> the relativecontributions <strong>of</strong> supply from different types <strong>of</strong> aggregate. This is important because thedifferent types are not always <strong>in</strong>terchangeable <strong>in</strong> terms <strong>of</strong> their suitability for different enduses. It is especially important <strong>in</strong> terms <strong>of</strong> the dist<strong>in</strong>ction between ‘hard rock’ aggregates(such as Carboniferous Limestone, Granite <strong>and</strong> Dolerite) <strong>and</strong> the much weaker materialsgenerally produced from younger rock types such as the Carboniferous s<strong>and</strong>stones with<strong>in</strong>the Forest <strong>of</strong> Dean, the Jurassic Limestones, <strong>and</strong> the Cretaceous Chalk <strong>and</strong> Greens<strong>and</strong>.The latter are referred to here as ‘weak rock’ aggregates <strong>and</strong> are generally produced as aby-product <strong>of</strong> build<strong>in</strong>g stone extraction. Included <strong>in</strong> the latter group are a small number <strong>of</strong>Devonian slate quarries where, <strong>in</strong> contrast to other build<strong>in</strong>g stone quarries, the ‘waste’ by-Capita Symonds Limited page 8 June 2005

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