Hostname: page-component-586b7cd67f-tf8b9 Total loading time: 0 Render date: 2024-11-27T19:37:06.687Z Has data issue: false hasContentIssue false
  • English
  • Français

The chalky till at Barrington, near Cambridge, and its connection with other Quaternary deposits in southern Cambridgeshire and adjoining areas

Published online by Cambridge University Press:  01 May 2009

P. G. Hoare  and
E. R. Connell
P. G. Hoare
Affiliation:
School of Geography, Cambridgeshire College of, Arts and Technology, Collier Road, Cambridge
E. R. Connell
Affiliation:
Department of Geography, University of Aberdeen, St Mary's, Old Aberdeen, Scotland
Get access Rights & Permissions [Opens in a new window]

Summary

The current belief in a single chalky till glaciation of eastern England is upheld by a detailed examination of a section at Barrington which had been said to reveal two such tills. An attempt is made to arrange the glacial, periglacical and interglacial beds of southern Cambridgeshire into stratigraphic order and to place them within Quaternary stages. The study concludes with a consideration of the fabric data that were used to support the claim that two major chalk-rich tills occur in East Anglia. Till mineralization is reported in the area for the first time.

Type
Articles
Information
Geological Magazine , Volume 118 , Issue 5 , September 1981 , pp. 463 - 476
Copyright
Copyright © Cambridge University Press 1981

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Andrews, J. T. 1971. Techniques of till fabric analysis. British Geomorphological Research Group Tech. Bull. 6. Norwich: Geo Abstracts.Google Scholar
Andrews, J. T. & King, C. A. M. 1968. Comparative till fabrics and till fabric variability in a till sheet and a drumlin: a small-scale study Proc. Yorks. geol. Soc. 36, 435–61.CrossRefGoogle Scholar
Baker, C. A. 1976. Late Devensian periglacial phenomena in the upper Cam valley, north Essex. Proc. Geol. Ass. 87, 285–306.CrossRefGoogle Scholar
Bascomb, C. L. 1961. A calcimeter for routine use on soil samples. Chemy Ind. 1826–7.Google Scholar
Boulton, G. S. 1976. A genetic classification of tills and criteria for distinguishing tills of different origin Geografia 12, 65–80.Google Scholar
Boulton, G. S. & Paul, M. A. 1976. The influence of genetic processes on some geotechnical properties of glacial tills. Q. Jl Engng Geol. 9, 159–94.CrossRefGoogle Scholar
Bristow, C. R. & Cox, F. C. 1973. The Gipping till: a reappraisal of East Anglian glacial stratigraphy Q. Jl geol. Soc. Lond. 129, 1–37.CrossRefGoogle Scholar
Butzer, K. W. & Isaac, G. L. (eds). 1975. After the Australopithecines: Stratigraphy, Ecology and Culture Change in the Middle Pleistocene. The Hague: Mouton.CrossRefGoogle Scholar
Cox, F. C. & Nickless, E. F. P. 1972. Some aspects of the glacial history of central Norfolk Bull. geol. Surv. G.B. 42, 79–98.Google Scholar
Curray, J. R. 1956. The analysis of two-dimensional orientation data. J. Geol. 64, 117–31.CrossRefGoogle Scholar
Fisher, O. 1879. On a mammaliferous deposit at Barrington, near Cambridge Q. Jl geol. Soc. Lond. 35, 670–7.CrossRefGoogle Scholar
Fisher, O. 1911. The land-ice hypothesis Geol. Mag. 8, 238–9.CrossRefGoogle Scholar
Fuller, M. D. 1962. A magnetic fabric in till. Geol. Mag. 99, 233–7.CrossRefGoogle Scholar
Gibbard, P. L. 1977. Pleistocene history of the Vale of St Albans. Phil. Trans. R. Soc. Lond. B 280, 445–83.Google Scholar
Gibbard, P. L. & Stuart, A. J. 1975. Flora and vertebrate fauna of the Barrington Beds Geol. Mag. 112, 493–501.CrossRefGoogle Scholar
Harris, S. A. 1968. Till fabrics and speed of movement of the Arapahoe glacier, Colorado. Prof. Geogr. 20, 195–8.CrossRefGoogle Scholar
Hawkes, L. 1943. The erratics of the Cambridge Greensand – their nature provenance and mode of transport. Q. Jl geol. Soc. Lond. 99, 93–104.CrossRefGoogle Scholar
Hill, A. R. 1971. The internal composition and structure of drumlins in north Down and south Antrim, Northern Ireland. Geogr. Annlr 53A, 14–31.CrossRefGoogle Scholar
Holmes, C. D. 1941. Till fabric Bull. geol. Soc. Am. 52, 1299–1354.CrossRefGoogle Scholar
Holmes, S. C. A. 1971. The geological mapper and the employment of his results, as illustrated in some areas of southern England. Proc. Geol. Ass. 82, 161–86.CrossRefGoogle Scholar
Home, H. 1903. On a transported mass of Ampthill Clay in the boulder-clay at Biggleswade (Bedfordshire) Q. J1 geol. Soc. Lond. 59, 375–81.CrossRefGoogle Scholar
Hughes, T. McK. 1911. Excursion to Cambridge and Barrington Proc. Geol. Ass. 22, 268–78.CrossRefGoogle Scholar
Hughes, T. McK. 1916. The Gravels of East Anglia. Cambridge University Press.Google Scholar
King, W. B. R. 1952. Pleistocene sections at Barrington Geol. Mag. 89, 382–3.CrossRefGoogle Scholar
King, W. B. R. 1955. The Pleistocene epoch in England Q. Jl geol. Soc. Lond. 111, 187–208.CrossRefGoogle Scholar
Legget, R. F. (ed.). 1976. Glacial Till. Ottawa: Royal Society of Canada.Google Scholar
Mitchell, G. F., Penny, L. F., Shotton, F. W. & West, R. G. 1973. A correlation of Quaternary deposits in the British Isles. Geol. Soc. Lond., Spec. Rep. 4.Google Scholar
Norris, G. 1962. Some glacial deposits and their relation to the Hippopotamus–bearing beds at Barrington, Cambridgeshire Geol. Mag. 99, 97–118.CrossRefGoogle Scholar
Perrin, R. M. S., Davies, H. & Fysh, M. D. 1973. Lithology of the Chalky Boulder Clay Nature, Lond. 245, 101–4.Google Scholar
Perrin, R. M. S., Davies, H. & Fysh, M. D. 1974. Distribution of late Pleistocene aeolian deposits in eastern and southern England Nature, Lond. 248, 320–3.CrossRefGoogle Scholar
Perrin, R. M. S., Rose, J. & Davies, H. 1979. The distribution, variation and origins of pre-Devensian tills in eastern England. Phil. Trans. R. Soc. Lond. B 287, 535–70.Google Scholar
Rose, J. 1974. Small-scale spatial variability of some sedimentary properties of lodgement till and slumped till Proc. Geol. Ass. 85, 239–58.CrossRefGoogle Scholar
Shotton, F. W. (ed.) 1977. British Quaternary Studies: Recent Advances. Oxford: Oxford University Press.Google Scholar
Sparks, B. W. 1952(a). Notes on some Pleistocene sections at Barrington, Cambridgeshire. Geol. Mag. 89, 163–74.CrossRefGoogle Scholar
Sparks, B. W. 1952(b). Reply to letter on Pleistocene sections at Barrington by W. B. R. King (1952) (q.v.). Geol. Mag. 89, 383–4.Google Scholar
Steers, J. A. (ed.). 1965. The Cambridge Region 1965. London: British Association for the Advancement of Science.Google Scholar
Sutcliffe, A. J. 1960. Joint Mitnor Cave, Buckfastleigh Trans. Proc. Torquay nat. Hist. Soc. 13, 1–26.Google Scholar
Taylor, A. G. 1978. Thermokarst depressions in southern Cambridgeshire Quaternary Newsl. 26, 1–2.Google Scholar
West, R. G. 1963. Problems of the British Quaternary. Proc. Geol. Ass. 74, 147–86.CrossRefGoogle Scholar
West, R. G. 1973. A state of confusion in Norfolk Pleistocene stratigraphy Bull. geol. Soc. Norfolk 23, 3–9.Google Scholar
West, R. G. & Donner, J. J. 1956. The glaciations of East Anglia and the east Midlands: a differentiation based on stone-orientation measurements of the tills Q. Jl geol. Soc. Lond. 112, 69–91.CrossRefGoogle Scholar
Wymer, J. J. 1974. Clactonian and Acheulian industries in Britain - their chronology and significance Proc. Geol. Ass. 85, 391–421.CrossRefGoogle Scholar