Hostname: page-component-cd9895bd7-lnqnp Total loading time: 0 Render date: 2024-12-24T16:33:07.148Z Has data issue: false hasContentIssue false
  • English
  • Français

A Note on the Pleistocene Deposit at Grantchester, Cambridgeshire

Published online by Cambridge University Press:  01 May 2009

B. W. Sparks
B. W. Sparks
Affiliation:
Department of Geography, University of Cambridge.
Get access Rights & Permissions [Opens in a new window]

Abstract

Examination of material from this locality kept in the Sedgwick Museum since 1881 has revealed much more about its molluscan fauna, especially about the frequency of species. It seems to have been a deposit of the main river Cam in the middle of the Last Interglacial.

Type
Articles
Information
Geological Magazine , Volume 101 , Issue 4 , 24 August 1964 , pp. 334 - 339
Copyright
Copyright © Cambridge University Press 1964

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

REFERENCES

Hughes, MrsMcKenny, . 1888. On the Mollusca of the Pleistocene gravels in the neighbourhood of Cambridge. Geol. Mag., 25, 193–207.CrossRefGoogle Scholar
Kennard, A. S., and Woodward, B. B., 1922. The post–Pliocene non–marine Mollusca of the east of England. Proc. Geol. Ass. Lond., 33, 104–42.Google Scholar
Kerney, M. P., 1959. An interglacial tufa near Hitchin, Hertfordshire. Proc. Geol. Ass. Lond., 70, 322–37.Google Scholar
Marr, J. E., 1920. The Pleistocene deposits around Cambridge. Quart. J. geol. Soc. Lond., 75, 204–42.CrossRefGoogle Scholar
Sparks, B. W., 1957. The evolution of the relief of the Cam valley. Geogr. J., 123, 188–207.Google Scholar
Sparks, B. W., 1961. The ecological interpretation of Quaternary non-marine Mollusca. Proc. Linn. Soc. Lond., 172, 71–80.CrossRefGoogle Scholar
Sparks, B. W., and West, R. G., 1959. The palaeoecology of the interglacial deposits at Histon Road, Cambridge. Eiszeitalter und Gegenwart, 10, 123–43.Google Scholar