EdenteV2, Istex, Corpus, bibRecord, 007198

The origin and development of the travertines and associated thermal waters at Matlock Bath, Derbyshire

Identifieur interne : 007198 ( Istex/Corpus ); précédent : 007197; suivant : 007199

The origin and development of the travertines and associated thermal waters at Matlock Bath, Derbyshire

Auteurs : Allan Pentecost

Source :

Proceedings of the Geologists' Association [ 0016-7878 ] ; 1999.

RBID : ISTEX:E55F3937C1C0237BA9E89F5CCF5AE06999DF58C4

English descriptors

KwdEn :
- Alga vaucheria, Aquatic plant photosynthesis, Bath cascade, Bath city council, Bath hotel, Bath profile, Bath spring, Bath springs, British isles, British travertines, Calcareous tufa, Calcite, Calcite saturation quotients, Calcium carbonate, Carbon dioxide, Carbonate, Carboniferous, Carboniferous limestone, Cascade, Cascade front, Chemical composition, Chemical compositions, Comm, Craton euron, Crystal growth, Deposit, Deposit travertine, Deposition, Derbyshire, Derbyshire dome, Derwent, Dioxide, East bank, Edmunds, Flindall hayes, Grand pavilion, Groundwater, High levels, Hydrothermal systems, Inactive travertines, Ionic composition, Isotope, Isotopic equilibrium, Karst, Karst waters, Lava, Limestone, Lower lava, Magnesian calcite, Major cations, Major ions, Masson hill, Matlock, Matlock bath, Matlock bath area, Matlock bath travertines, Matlock dale, Meteogene travertines, Micrite, Millstone grit, Modem, Modem travertine, Modem travertines, Modern travertines, Monsal dale limestone, Moss cratoneuron commutatum, Older travertines, Open framework, Palisade, Palisade calcite, Peak district, Peak district mines, Pedley, Pentecost, Pentecost table, Pers, Pollen samples, Precipitation, Quarried, Quarried block, River derwent, Scale bars, Secondary deposition, Secondary sparite, Sedimentary petrology, Several directions, Small pond, Sparite, Specific conductivity, Spring waters, Stable isotope analyses, Thermal springs, Thermal water, Thermal waters, Travertine, Travertine deposition, Travertine deposits, Travertine fabric, Travertine samples, Travertine section, Travertines, Tufa, Water flow, Water flows, Water temperature, Wragg sough.
Teeft :
- Alga vaucheria, Aquatic plant photosynthesis, Bath cascade, Bath city council, Bath hotel, Bath profile, Bath spring, Bath springs, British isles, British travertines, Calcareous tufa, Calcite, Calcite saturation quotients, Calcium carbonate, Carbon dioxide, Carbonate, Carboniferous, Carboniferous limestone, Cascade, Cascade front, Chemical composition, Chemical compositions, Comm, Craton euron, Crystal growth, Deposit, Deposit travertine, Deposition, Derbyshire, Derbyshire dome, Derwent, Dioxide, East bank, Edmunds, Flindall hayes, Grand pavilion, Groundwater, High levels, Hydrothermal systems, Inactive travertines, Ionic composition, Isotope, Isotopic equilibrium, Karst, Karst waters, Lava, Limestone, Lower lava, Magnesian calcite, Major cations, Major ions, Masson hill, Matlock, Matlock bath, Matlock bath area, Matlock bath travertines, Matlock dale, Meteogene travertines, Micrite, Millstone grit, Modem, Modem travertine, Modem travertines, Modern travertines, Monsal dale limestone, Moss cratoneuron commutatum, Older travertines, Open framework, Palisade, Palisade calcite, Peak district, Peak district mines, Pedley, Pentecost, Pentecost table, Pers, Pollen samples, Precipitation, Quarried, Quarried block, River derwent, Scale bars, Secondary deposition, Secondary sparite, Sedimentary petrology, Several directions, Small pond, Sparite, Specific conductivity, Spring waters, Stable isotope analyses, Thermal springs, Thermal water, Thermal waters, Travertine, Travertine deposition, Travertine deposits, Travertine fabric, Travertine samples, Travertine section, Travertines, Tufa, Water flow, Water flows, Water temperature, Wragg sough.

Abstract

An investigation has been made of the hydrochemistry of the five thermal springs at Matlock Bath and the geochemistry of the associated travertines. The thermal waters are shown to have a common source and originate from precipitation which has equilibrated with a soil atmosphere which has descended through Carboniferous Limestone at a depth probably no greater than 0.5 km. The springs issue below a basalt lava at Matlock Bath at 20°C.Two springs deposit travertine (calcareous tufa) which covers an area of about 6 ha. The travertines consist of low magnesian calcite but with high levels of Sr, Pb and Zn . Their δ13C and δ18O values indicate deposition at or close to isotopic equilibrium with the springwater and confirm a soil-origin of the CO2 in the percolation water. The travertines form around the moss Cratoneuron commutatum which provides an open framework and is ultimately cemented with microspar to form a tough low-porosity deposit. Inactive travertines at the New Bath contain molluscan and pollen assemblages suggesting an open nitrophile woodland environment probably of Atlantic age or later.

Url:

https://api.istex.fr/document/E55F3937C1C0237BA9E89F5CCF5AE06999DF58C4/fulltext/pdf

DOI: 10.1016/S0016-7878(99)80072-8

Links to Exploration step

ISTEX:E55F3937C1C0237BA9E89F5CCF5AE06999DF58C4

Le document en format XML

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<term>Bath hotel</term>
<term>Bath profile</term>
<term>Bath spring</term>
<term>Bath springs</term>
<term>British isles</term>
<term>British travertines</term>
<term>Calcareous tufa</term>
<term>Calcite</term>
<term>Calcite saturation quotients</term>
<term>Calcium carbonate</term>
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<term>Carboniferous limestone</term>
<term>Cascade</term>
<term>Cascade front</term>
<term>Chemical composition</term>
<term>Chemical compositions</term>
<term>Comm</term>
<term>Craton euron</term>
<term>Crystal growth</term>
<term>Deposit</term>
<term>Deposit travertine</term>
<term>Deposition</term>
<term>Derbyshire</term>
<term>Derbyshire dome</term>
<term>Derwent</term>
<term>Dioxide</term>
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<term>Hydrothermal systems</term>
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<term>Peak district mines</term>
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<term>Pentecost</term>
<term>Pentecost table</term>
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<term>Pollen samples</term>
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<term>River derwent</term>
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<front><div type="abstract">An investigation has been made of the hydrochemistry of the five thermal springs at Matlock Bath and the geochemistry of the associated travertines. The thermal waters are shown to have a common source and originate from precipitation which has equilibrated with a soil atmosphere which has descended through Carboniferous Limestone at a depth probably no greater than 0.5 km. The springs issue below a basalt lava at Matlock Bath at 20°C.Two springs deposit travertine (calcareous tufa) which covers an area of about 6 ha. The travertines consist of low magnesian calcite but with high levels of Sr, Pb and Zn . Their δ13C and δ18O values indicate deposition at or close to isotopic equilibrium with the springwater and confirm a soil-origin of the CO2 in the percolation water. The travertines form around the moss Cratoneuron commutatum which provides an open framework and is ultimately cemented with microspar to form a tough low-porosity deposit. Inactive travertines at the New Bath contain molluscan and pollen assemblages suggesting an open nitrophile woodland environment probably of Atlantic age or later.</div>
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<abstract>An investigation has been made of the hydrochemistry of the five thermal springs at Matlock Bath and the geochemistry of the associated travertines. The thermal waters are shown to have a common source and originate from precipitation which has equilibrated with a soil atmosphere which has descended through Carboniferous Limestone at a depth probably no greater than 0.5 km. The springs issue below a basalt lava at Matlock Bath at 20°C.Two springs deposit travertine (calcareous tufa) which covers an area of about 6 ha. The travertines consist of low magnesian calcite but with high levels of Sr, Pb and Zn . Their δ13C and δ18O values indicate deposition at or close to isotopic equilibrium with the springwater and confirm a soil-origin of the CO2 in the percolation water. The travertines form around the moss Cratoneuron commutatum which provides an open framework and is ultimately cemented with microspar to form a tough low-porosity deposit. Inactive travertines at the New Bath contain molluscan and pollen assemblages suggesting an open nitrophile woodland environment probably of Atlantic age or later.</abstract>
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<json:string>see summary in Pentecost, 1993</json:string>
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<json:string>quoted in Stephen s, 1929</json:string>
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<json:string>Edmunds, 1971</json:string>
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<json:string>Usdowski et al., 1979</json:string>
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<json:string>Usdowski, Hoefs & Menschel, 1979</json:string>
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<json:string>see Julia, 1983</json:string>
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<json:string>de Capitani, Fiorentine & Terrani, 1974</json:string>
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<json:string>Henley, Truesdell, Barton & Whitney, 1984</json:string>
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<abstract><p>An investigation has been made of the hydrochemistry of the five thermal springs at Matlock Bath and the geochemistry of the associated travertines. The thermal waters are shown to have a common source and originate from precipitation which has equilibrated with a soil atmosphere which has descended through Carboniferous Limestone at a depth probably no greater than 0.5 km. The springs issue below a basalt lava at Matlock Bath at 20°C.Two springs deposit travertine (calcareous tufa) which covers an area of about 6 ha. The travertines consist of low magnesian calcite but with high levels of Sr, Pb and Zn . Their δ13C and δ18O values indicate deposition at or close to isotopic equilibrium with the springwater and confirm a soil-origin of the CO2 in the percolation water. The travertines form around the moss Cratoneuron commutatum which provides an open framework and is ultimately cemented with microspar to form a tough low-porosity deposit. Inactive travertines at the New Bath contain molluscan and pollen assemblages suggesting an open nitrophile woodland environment probably of Atlantic age or later.</p>
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<head><ce:title>The origin and development of the travertines and associated thermal waters at Matlock Bath, Derbyshire</ce:title>
<ce:author-group><ce:author><ce:given-name>Allan</ce:given-name>
<ce:surname>Pentecost</ce:surname>
</ce:author>
<ce:affiliation><ce:textfn>Division of Life Sciences, King's College London, Campden Hill Road, London W8 7 AH.</ce:textfn>
</ce:affiliation>
</ce:author-group>
<ce:date-received day="16" month="6" year="1998"></ce:date-received>
<ce:date-accepted day="11" month="12" year="1998"></ce:date-accepted>
<ce:abstract id="ab1"><ce:abstract-sec><ce:simple-para>An investigation has been made of the hydrochemistry of the five thermal springs at Matlock Bath and the geochemistry of the associated travertines. The thermal waters are shown to have a common source and originate from precipitation which has equilibrated with a soil atmosphere which has descended through Carboniferous Limestone at a depth probably no greater than 0.5 km. The springs issue below a basalt lava at Matlock Bath at 20°C.</ce:simple-para>
<ce:simple-para>Two springs deposit travertine (calcareous tufa) which covers an area of about 6 ha. The travertines consist of low magnesian calcite but with high levels of Sr, Pb and Zn . Their δ<ce:sup>13</ce:sup>
C and δ<ce:sup>18</ce:sup>
O values indicate deposition at or close to isotopic equilibrium with the springwater and confirm a soil-origin of the CO<ce:inf>2</ce:inf>
 in the percolation water. The travertines form around the moss Cratoneuron commutatum which provides an open framework and is ultimately cemented with microspar to form a tough low-porosity deposit. Inactive travertines at the New Bath contain molluscan and pollen assemblages suggesting an open nitrophile woodland environment probably of Atlantic age or later.</ce:simple-para>
</ce:abstract-sec>
</ce:abstract>
</head>
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<mods version="3.6"><titleInfo lang="en"><title>The origin and development of the travertines and associated thermal waters at Matlock Bath, Derbyshire</title>
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<titleInfo type="alternative" lang="en" contentType="CDATA"><title>The origin and development of the travertines and associated thermal waters at Matlock Bath, Derbyshire</title>
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<name type="personal"><namePart type="given">Allan</namePart>
<namePart type="family">Pentecost</namePart>
<affiliation>Division of Life Sciences, King's College London, Campden Hill Road, London W8 7 AH.</affiliation>
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<abstract>An investigation has been made of the hydrochemistry of the five thermal springs at Matlock Bath and the geochemistry of the associated travertines. The thermal waters are shown to have a common source and originate from precipitation which has equilibrated with a soil atmosphere which has descended through Carboniferous Limestone at a depth probably no greater than 0.5 km. The springs issue below a basalt lava at Matlock Bath at 20°C.Two springs deposit travertine (calcareous tufa) which covers an area of about 6 ha. The travertines consist of low magnesian calcite but with high levels of Sr, Pb and Zn . Their δ13C and δ18O values indicate deposition at or close to isotopic equilibrium with the springwater and confirm a soil-origin of the CO2 in the percolation water. The travertines form around the moss Cratoneuron commutatum which provides an open framework and is ultimately cemented with microspar to form a tough low-porosity deposit. Inactive travertines at the New Bath contain molluscan and pollen assemblages suggesting an open nitrophile woodland environment probably of Atlantic age or later.</abstract>
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<identifier type="ISSN">0016-7878</identifier>
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<detail type="issue"><number>3</number>
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<extent unit="issue-pages"><start>193</start>
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<extent unit="pages"><start>217</start>
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The origin and development of the travertines and associated thermal waters at Matlock Bath, Derbyshire

The origin and development of the travertines and associated thermal waters at Matlock Bath, Derbyshire

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