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Meerbrook Sough

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Journal Article
Published: 01 May 2007
Quarterly Journal of Engineering Geology and Hydrogeology (2007) 40 (2): 123–135.
...M.G. Shepley Abstract The flow hydrograph of a large mine drainage adit, the Meerbrook Sough, has been analysed to determine the large-scale hydraulic behaviour of the artificially drained Carboniferous Limestone aquifer. A conceptual model has been constructed using available hydrological...
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Image
The outlet at the Meerbrook Sough tail. The photograph is used with permission from Roger James.
Published: 01 May 2007
Fig. 4 The outlet at the Meerbrook Sough tail. The photograph is used with permission from Roger James.
Image
Cross-section of the Meerbrook Sough catchment. The geology is simplified from Frost & Smart (1979).
Published: 01 May 2007
Fig. 3 Cross-section of the Meerbrook Sough catchment. The geology is simplified from Frost & Smart (1979) .
Image
Comparison of simulated flows and measured flows of the Meerbrook Sough: (a) total flow range; (b) seasonal detail.
Published: 01 May 2007
Fig. 8 Comparison of simulated flows and measured flows of the Meerbrook Sough: ( a ) total flow range; ( b ) seasonal detail.
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Comparison of simulated flows and measured flows of the Meerbrook Sough: (a) total flow range; (b) seasonal detail.
Published: 01 May 2007
Fig. 8 Comparison of simulated flows and measured flows of the Meerbrook Sough: ( a ) total flow range; ( b ) seasonal detail.
Image
Comparison of Meerbrook Sough flows and gauged surface water flows from a predominantly Carboniferous Limestone catchment in the Derbyshire Peak District.
Published: 01 May 2007
Fig. 5 Comparison of Meerbrook Sough flows and gauged surface water flows from a predominantly Carboniferous Limestone catchment in the Derbyshire Peak District.
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The geology and hydrology of the Meerbrook Sough catchment. Data are taken from Stephens (1929), Edmunds (1971), Frost & Smart (1979), Aitkenhead et al. (1985), Rieuwerts (1987), Gunn (1998), Ford (2005), Severn Trent Water Authority records and the Environment Agency Hydrometric Archive.
Published: 01 May 2007
Fig. 2 The geology and hydrology of the Meerbrook Sough catchment. Data are taken from Stephens (1929) , Edmunds (1971) , Frost & Smart (1979) , Aitkenhead et al . (1985) , Rieuwerts (1987) , Gunn (1998) , Ford (2005) , Severn Trent Water Authority records and the Environment Agency
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Comparison of Carboniferous Limestone groundwater levels close to the Meerbrook Sough.
Published: 01 May 2007
Fig. 6 Comparison of Carboniferous Limestone groundwater levels close to the Meerbrook Sough.
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Comparison of simulated groundwater heads and observed groundwater levels within the catchment of the Meerbrook Sough.
Published: 01 May 2007
Fig. 7 Comparison of simulated groundwater heads and observed groundwater levels within the catchment of the Meerbrook Sough.
Journal Article
Published: 01 February 2008
Quarterly Journal of Engineering Geology and Hydrogeology (2008) 41 (1): 121–122.
...F.C. Brassington 1 11 2007 11 9 2007 © 2008 The Geological Society of London 2008 F.C. Brassington writes: Shepley is to be congratulated on his detailed description of the Meerbrook Sough and analysis of the groundwater discharge from this abandoned mine drainage system...
Journal Article
Published: 01 February 2008
Quarterly Journal of Engineering Geology and Hydrogeology (2008) 41 (1): 119–120.
... with the Buxton waters. Shepley (2007 , p. 130) also suggests that the thermal waters that enter Meerbrook Sough circulated to ‘depths greater than 600 m below surface’, which agrees well with the model of Gunn et al . (2006) in which Matlock-type waters are shown as migrating to c . 800 m depth...
Journal Article
Published: 01 May 2009
Quarterly Journal of Engineering Geology and Hydrogeology (2009) 42 (2): 211–225.
... to deeper valleys with lower base levels ( Rieuwerts 1981 ). This has increased the easterly hydraulic gradient across the region. Edmunds (1971, p. 5) observed that ‘four soughs, Magpie (SK 179 696), Meerbrook (SK 327 552), Yatestoop (SK 264 626) and Hillcarr (SK 257 637) have flows in excess of 500 l...
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Journal Article
Published: 31 January 2018
Journal of the Geological Society (2018) 175 (3): 443–463.
.... Ford & Gunn (2008) suggested that the Brassington area is primarily drained via the mineral vein fissures that are under-drained by Meerbrook Sough ( Shepley 2007 ). This indicates that the Miocene drainage was also strongly guided by mineral veins. To date, however, a satisfactory explanation...
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Series: Geological Society, London, Special Publications
Published: 01 January 2004
DOI: 10.1144/GSL.SP.2004.225.01.09
EISBN: 9781862394735
... to the river for a number of large collieries to the west of Newcastle city Galloway (1898, p. 268) 1772 Meerbrook Sough Derbyshire Lead Driven to under-drain mines in the Cromford and Wirksworth areas, it was 3 km long by 1805, and was later driven further between 1842 and 1882. Continues to yield...
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