Hostname: page-component-cd9895bd7-7cvxr Total loading time: 0 Render date: 2024-12-26T06:33:41.254Z Has data issue: false hasContentIssue false
  • English
  • Français

On the Early Pebble Gravels of the Thames Basin from the Hertfordshire-Essex Border to Clacton-on-Sea

Published online by Cambridge University Press:  01 May 2009

S. Hazzledine Warren
S. Hazzledine Warren
Affiliation:
Forest View Road, Loughton, Essex
Get access Rights & Permissions [Opens in a new window]

Abstract

The erratic rocks of the early pebble gravels are similar to those of the Oxford plateau drift, and reasons are given for concluding that they belong to the drifts of the proto-Thames, and are earlier than the southward diversion of that river by an advancing ice-sheet. Comparisons with the constituents of the later deposits of the Clacton channel are also discussed.

Type
Articles
Information
Geological Magazine , Volume 94 , Issue 1 , February 1957 , pp. 40 - 46
Copyright
Copyright © Cambridge University Press 1957

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

Baden-Powell, D. W. F., 1951. The age of the interglacial deposits at Swanscombe. Geol. Mag., lxxxviii, 344–356.CrossRefGoogle Scholar
Buckland, W., 1823. “Reliquiae Diluvianae,” p. 249; map pl. 27.Google Scholar
Gregory, J. W., 1922. Evolution of the Essex rivers and of the Lower Thames. Colchester, 68 pp.CrossRefGoogle Scholar
Oakley, K. P., and Leakey, Mary, 1938. Report on excavations at Jaywick Sands, Essex (1934). Proc. Prehist. Soc. for 1937, 217–260.Google Scholar
Salter, A. E., 1905. On the superficial deposits of Central and parts of Eastern England. Proc. Geol. Assoc., xix, 1–56.CrossRefGoogle Scholar
Sandford, K. S., 1929. The erratic rocks and the age of the southern limit of glaciation in the Oxford district. Quart. Journ. Geol. Soc., lxxxv, 359–388.CrossRefGoogle Scholar
Sherlock, R. L., 1924. The superficial deposits of South Buckinghamshire and South Hertfordshire and the old course of the Thames. Proc. Geol. Assoc., xxxv, 1–28.CrossRefGoogle Scholar
Solomon, J. D., 1935. The Westleton Series of East Anglia: its age, distribution, and relations. Quart. Journ. Geol. Soc. London, xci, 216–238.CrossRefGoogle Scholar
Warren, S. Hazzledine, 1940. Geological and prehistoric traps. Essex Nat., xxvii, 2–19.Google Scholar
Warren, S. Hazzledine, 1945. Some geologic and prehistoric records on the north-western border of Essex. Essex Nat., xxvii, 273–280.Google Scholar
Warren, S. Hazzledine, 1951. The Clacton flint industry: a new interpretation. Proc. Geol. Assoc., lxii, 107–135.CrossRefGoogle Scholar
Warren, S. Hazzledine and Baden-Powell, D. F. W., 1955. The Clacton channel deposits. Quart. Journ. Geol. Soc. London, cxi, 283–307.CrossRefGoogle Scholar
Whitaker, W., 1877. The geology of the eastern end of Essex (Walton Naze and Harwich). Mem. Geol. Surv., 32 pp.Google Scholar
Wells, A. K., and Wooldridge, S. W., 1923. Notes on the geology of Epping Forest. Proc. Geol. Assoc., xxxiv, 244–252.CrossRefGoogle Scholar
Wooldridge, S. W., 1927. The Pliocene history of the London Basin. Proc. Geol. Assoc., xxxviii, 49–132.CrossRefGoogle Scholar
Wooldridge, S. W., 1927. The Pliocene period in western Essex and the pre-glacial topography of the district. Essex Nat., xxi, 247–268.Google Scholar
Wooldridge, S. W., 1928. The 200-foot platform in the London Basin. Proc. Geol. Assoc., xxxix, 1–26.CrossRefGoogle Scholar
Wooldridge, S. W., 1938. The glaciation of the London Basin and the evolution of the Lower Thames drainage system. Quart. Journ. Geol. Soc., xciv, 627–667.CrossRefGoogle Scholar