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Hotwells England

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Journal Article
Published: 30 July 2013
Quarterly Journal of Engineering Geology and Hydrogeology (2013) 46 (3): 267–279.
...C. McCann; A. C. Mann; D. M. McCann; G. A. Kellaway Abstract The thermal springs of Bath, England, produce 1.25 Ml day −1 of water at 46.5 °C. The spring at Hotwells, Bristol, England, 15 km to the west, is estimated to produce between 0.17 and 0.39 Ml day −1 of water at a temperature between 22.8...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2002
DOI: 10.1144/GSL.SP.2002.193.01.02
EISBN: 9781862394414
... Abstract The hot springs at Bath are the largest natural thermal source in Britain. Sustainable use of the waters for a spa requires maintenance of their temperature and flow rate. Together with smaller springs at Hotwells, Bristol, they form the outflow from a regional thermal aquifer...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2002
DOI: 10.1144/GSL.SP.2002.193.01.03
EISBN: 9781862394414
... Abstract The origin of the thermal springs of Bath (England) remains unknown. As part of a programme of research into the structure of the thermal aquifer, the Carboniferous Limestone, an urban reflection seismic survey has been carried out to explore the deep geology of the Bath area. Existing...
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Journal Article
Published: 01 July 2004
Geological Magazine (2004) 141 (4): 471–504.
...GAVIN R. T. WALL; HUGH C. JENKYNS Abstract In the eastern Mendip Hills, on the northern margin of the Wessex Basin, SW England, the Carboniferous Limestone is cut by numerous fissures that are filled with Mesozoic sediments (sedimentary dykes, neptunian dykes). The fissures contain a record...
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Series: Geological Society, London, Geology of Series, Geological Society, London, Geology of Series
Published: 01 January 2006
DOI: 10.1144/GOEWP.9
EISBN: 9781862393882
... Abstract The structural evolution of England and Wales during the Carboniferous was primarily a consequence of an oblique (dextral) collision between Gondwana and Laurussia ( Warr 2000 ). Several phases can be recognized. The Rhenohercynian Ocean opened during Early–Mid Devonian regional bacK...
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Journal Article
Journal: AAPG Bulletin
Published: 01 December 1972
AAPG Bulletin (1972) 56 (12): 2392–2414.
... of terrigenous influx toward the type locality at Bristol, England. These units also contain distinctive biotic and geochemical constituents that support paleoenvironmental interpretations. Carbonate sediments were deposited on a shallow subsiding shelf under poorly oxygenated conditions, in a warm humid...
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Journal Article
Published: 17 May 2019
Quarterly Journal of Engineering Geology and Hydrogeology (2019) 52 (4): 557–562.
... are generally more saline than seawater and, while disposal of spent brine could take place into the sea under favourable conditions, re-injection would be necessary for inland sites. In the UK, these are associated exclusively with the Carboniferous Limestone of England and Wales (there are no known...
FIGURES
Journal Article
Published: 01 July 2007
Geological Magazine (2007) 144 (4): 741–747.
... There are only five known occurrences of thermal springs in the UK, of which only that at Bath Spa exceeds the 30 °C defined by White (1957) as the lowest temperature at which a spring should be called hot. The springs at Hotwells (Bristol), Taff’s Well (Cardiff), and Buxton and Matlock Spa (Peak District...
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Journal Article
Published: 01 February 2000
Quarterly Journal of Engineering Geology and Hydrogeology (2000) 33 (1): 41–58.
...; Rollin 1986; Lee et al. 1987; Gebski et al. 1987). The mean of 26 heat flow measurements in the Hercynian granite batholith beneath southwest England is 117 ± 8 mW/m 2 . Maximum values of 101 mW/m 2 and 76 mW/m 2 have been recorded from the Caledonian granites in northern England and the Eastern...
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Journal Article
Published: 01 January 1986
Journal of the Geological Society (1986) 143 (1): 63–73.
... and memoir. The general resemblance between Permo-Carboniferous structures in the Bristol/Somerset coalfield and those of N France and western England was noted in the mid 19th century (Godwin-Austen 1856) and the possibility of intervening, concealed coalfields was proposed. Other notable, early...
Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2013
DOI: 10.1144/SP375.16
EISBN: 9781862396432
...; by the late 17th century there were over 400 identifiable mineral water sources dispersed throughout England, Scotland and Wales ( Osborne & Weaver 1996 ) and many of the associated villages could offer food and lodging. Spas reached the peak of their popularity during the 18th century. Many of the spa...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2007
DOI: 10.1144/SP281.6
EISBN: 9781862395299
.... In the 1840s a number of these had opened in England: Queen's College, London (in 1847) and Bedford College, London (in 1849) ( Burek 2007 ), and these were followed by further examples: Girton College, Oxford, and Newnham College, Cambridge. In the United States, similar women's colleges were providing...
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Journal Article
Published: 01 May 2008
Journal of Paleontology (2008) 82 (3): 595–603.
... – 150 . Batten , R. L. , 1966 , The Lower Carboniferous gastropod fauna from the Hotwells limestone of Compton Martin, Somerset : Palaeontographical Society Monographs , 119 . 53 – 109 . Blodgett , R. B. , 1998 , Emsian (late Early Devonian) fossils indicate a Siberian origin...
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Journal Article
Journal: PALAIOS
Published: 01 November 2009
PALAIOS (2009) 24 (11): 756–771.
... States ( Hoare and Pojeta, 2006 ), and (4) the Early Devonian of southeastern Australia ( Johnston 1993 )—and a fauna with calcareous shell preservation, (5) the Early Carboniferous of southwestern England, UK ( Mitchell, 1987 ). In analyzing these faunas, we compare the abundance and diversity...
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Journal Article
Published: 01 May 1972
Journal of the Geological Society (1972) 128 (3): 221–256.