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Limestone in Cheltenham clay

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Journal Article
Published: 01 December 1978
Journal of the Geological Society (1978) 135 (6): 611–627.
... along the escarpment between Chipping Campden and Wotton-under-Edge, but exposures away from this line are limited (Fig. 1). These rocks are represented by a variable series of coarse-grained limestones, marls and subordinate sands and clays, laid down in a shallow shelf sea in a lenticular sheet...
Journal Article
Published: 27 November 2014
Journal of the Geological Society (2015) 172 (1): 63–76.
... and ooidal limestone gravel, known as the Cheltenham Sand and Gravel, occur at the foot of the scarp around Cheltenham and north to Bredon Hill ( Fig. 4 ). These are thought to be composite solifluction and aeolian deposits (‘head’) of Devensian age ( Barron et al . 2002 ). In this study we have used...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1956
AAPG Bulletin (1956) 40 (11): 2689–2710.
... of kaolinite derived from the chemical weathering of the contiguous Paleozoic limestones (Robbins and Keller, 1952). Farther downflank and closer to the Cheltenham sea the diaspore gives way to kaolinite in the flint clay zone. The clay minerals here imply less leaching than occurred farther inland...
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Journal Article
Journal: AAPG Bulletin
Published: 01 September 1955
AAPG Bulletin (1955) 39 (9): 1753–1820.
... of the southern and eastern parts of the basin contain quartz-pebble conglomerate in two stratigraphic units. Recent studies by Glass and Siever (1951) have shown that some of the limestones are dolomitic. Clay ironstone is common in the shale as thin bands or nodules and there is a very little chert associated...
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Journal Article
Journal: AAPG Bulletin
Published: 01 September 1939
AAPG Bulletin (1939) 23 (9): 1374–1392.
..., are present above coal No. 2 and above the horizon of coal No. 5 but elsewhere in the northwestern part of the basin they are very rarely and only locally developed. Along the La Salle anticline the strata below coal No. 2 are represented by thick fireclay similar and equivalent to the Cheltenham clay...
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Journal Article
Journal: PALAIOS
Published: 01 October 2009
PALAIOS (2009) 24 (10): 627–637.
... the clays found in the quarry at Central. Wanless (1939 , 1962) correlated the Goose Lake clay with the more extensive Cheltenham Clay. Current usage by the Illinois State Geological Survey ( Jacobson, 2008 ) places the Cheltenham entirely in the Desmoinesian; it ranges from the Tradewater Formation...
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Journal Article
Published: 07 November 2013
Quarterly Journal of Engineering Geology and Hydrogeology (2013) 46 (4): 405–420.
... (1907–1909). Table 1. The principal building limestone sources of Britain (active quarries shown underlined) Period Group Formation Stone Name Quaternary Tufa; Dursley Tertiary Bembridge Limestone Quarr Stone London Clay Septarian nodules Upper Cretaceous...
FIGURES
Journal Article
Published: 01 January 2008
Journal of the Geological Society (2008) 165 (1): 85–103.
... and shelly limestones. The youngest formation is the Great Oolite, a bedded succession of calcareous and argillaceous units containing a greater amount of mud and clay than the underlying Inferior Oolite. The higher regions of the Cotswolds, around Stroud and Cheltenham, are capped by Inferior Oolite...
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Journal Article
Journal: AAPG Bulletin
Published: 01 February 1968
AAPG Bulletin (1968) 52 (2): 264–281.
.... In central Missouri, reef development in the Devonian has been studied in detail in the Callaway Limestone of the Middle Devonian ( Fraunfelter, 1964 ). The reefs are made up predominantly of patches composed of various corals. The low relief and the highly weathered surface of the Lower and Middle...
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Journal Article
Published: 08 April 2024
Proceedings of the Yorkshire Geological Society (2024) 65 (1-2): pygs2023-010.
... and praise Sedgwick's work, particularly that relating to the Whin Sill and the Magnesian Limestone ( Sedgwick 1827 , 1829 ). Another important contemporary scientist of national reputation, Prideaux John Selby (1783–1867) was born in Alnwick and later lived only a few miles north of the town. His...
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Journal Article
Published: 30 March 2021
Petroleum Geoscience (2021) 27 (3): petgeo2020-102.
.... 2014 ) is now reclassified as the top Svarte Formation in this study, based on new well data interpretation and correlation ( Fig. 3 ). Despite the change in stratigraphic allocation, this synrift package mainly comprises shale, marl and some limestones. Numerous NW–SE-trending faults formed within...
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Journal Article
Published: 01 June 1995
Journal of the Geological Society (1995) 152 (3): 481–485.
..., Cope et al. 1980). These sands thin northwards onto the Mendip axis, north of which they again thicken in the Bath-Cheltenham area (Bryant et al. 1988, fig. 1, adapted from Davies 1967). Overall the facies are 481 482 K . T. PICKERING MENDIP AXIS r p Leger m m Id Outcrop of Toarclan Aalenlan sands...
Journal Article
Published: 01 August 2010
Quarterly Journal of Engineering Geology and Hydrogeology (2010) 43 (3): 333–344.
... . Cambering and valley bulging, periglacial solifluction and late-glacial Coleoptera at Dowdeswell, near Cheltenham . Proceedings of the Geologists' Association , 113 , 291 – 300 . Hutchinson J.N. Gostelow T.P. 1976 . The development of an abandoned cliff in London Clay at Hadleigh...
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Journal Article
Published: 03 July 2019
Journal of the Geological Society (2019) 176 (6): 1136–1142.
... Group; CG, Clackmannan Group; LCG, Limestone Coal Group; LCF, Lower Limestone Formation; YG, Yoredale Group; n.g., number of analyses not given or not deciphered from source. Depths given estimated based on seam stratigraphy, shaft excavation depth or borehole data (where available). Vitrinite...
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Series: Geological Society, London, Special Publications
Published: 01 January 2013
DOI: 10.1144/SP375.16
EISBN: 9781862396432
... possible to drink the waters and an analysis provided by Cheltenham Borough Council is given in Table 1 . The Cheltenham waters are saline in character and originate in the Jurassic Lower Lias Clay. These rocks consist of grey mudstones and thin subordinate argillaceous limestones which are around 225 m...
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Journal Article
Published: 04 June 2019
Geological Magazine (2019) 156 (10): 1793–1804.
... of the manuscript. The study was financially supported by grants from the Natural Sciences and Engineering Research Council of Canada (NSERC). References Allen VT ( 1936 ) A mineralized spherulitic limestone in the Cheltenham Fireclay . American Mineralogist 21 , 369 – 73 . Becq-Giraudon...
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Journal Article
Published: 15 July 2015
Journal of the Geological Society (2015) 172 (6): 683–692.
.... The limestone containing the insects is slightly coarse, so the insects are often poorly preserved. The specimens consist of wings, wing fragments, complete insects and body parts ( Fig. 3 a–e ), and parts are separated from counterparts. For the rarer orders, it was straightforward to try to reunite parts...
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Series: Geological Society, London, Geology of Series
Published: 01 January 2006
DOI: 10.1144/GOEWP.14
EISBN: 9781862393882
... contain rich faunas of bivalves, gastropods, brachiopods and echinoids; corals occasionally flourished in shallow-water areas, particularly those fringing the land areas. Clays, sands and limestones are often arranged in cycles; the clays becoming progressively more silty upwards and the sands more...
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Journal Article
Published: 01 February 1985
Journal of the Geological Society (1985) 142 (1): 207–220.
... in the earth sciences 12-14 April 1984. Joint meeting of the Metamorphic studies Group and the Mineralogical Society Clay Mineralogy and Geochemistry Group held at the University of Bristol Diagenesis and low temperature metamorphism The transition from diagenesis to low temperature meta- morphism in the Alps...
Journal Article
Published: 01 May 2004
Journal of Sedimentary Research (2004) 74 (3): 355–365.
... of ferroan calcite. E) Crinoid ossicle from Lias, Cheltenham, U.K., specimen 38. Galleried stereom forming center of ossicle (upper right), labyrinthic stereom forming periphery of ossicle (lower left). F) Galleried stereom composed of nonporous Mg calcite (uniform dark gray); labyrinthic stereom...
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