Hostname: page-component-84b7d79bbc-g7rbq Total loading time: 0 Render date: 2024-07-27T21:02:03.454Z Has data issue: false hasContentIssue false
  • English
  • Français

Pleistocene Deposits on the West Side of the Malvern Hills

Published online by Cambridge University Press:  01 May 2009

R. W. Hey
R. W. Hey
Affiliation:
Sedgwick Museum, Cambridge.
Get access Rights & Permissions [Opens in a new window]

Abstract

A north-south valley west of the Malverns contains a variety of Pleistocene deposits, largely hidden by late Pleistocene solifluxion. Around Eastnor is a stony clay attributed to an ice-tongue that crossed the Malvern Hills from the Severn valley. Various sediments north of Eastnor are thought to have been laid down in a lake held up by this ice-tongue and fed by a stream diverted across the hills north of the Malverns by the main Severn valley glacier. The Upleadon Gravels south of Eastnor are attributed to water released from the lake when the ice-tongue melted. Both lake and glacier are correlated with the Woolridge Gravels and hence with the Penultimate Glaciation.

Type
Articles
Information
Geological Magazine , Volume 96 , Issue 5 , October 1959 , pp. 403 - 417
Copyright
Copyright © Cambridge University Press 1959

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

Dwerryhouse, A. R., and Miller, A. A., 1930. The glaciation of Clun Forest, Radnor Forest and some adjoining districts. Quart. Journ. Geol. Soc., lxxxvi, 96–129.Google Scholar
Gray, J. W., 1914. The drift deposits of the Malverns. Proc. Birmingham Nat. Hist. Phil. Soc., xiii, 1–18.Google Scholar
Gray, J. W., 1919. Notes on the Cotteswold-Malvern region during the Quaternary period. Proc. Cotteswold Nat. Field Club, xx, 99–141.Google Scholar
Grindley, H. E., 1921. Observations on the Midland drift as seen in two sand-pits at Mathon. Trans. Woolhope Nat. Field Club, 176–7.Google Scholar
Groom, T. T., 1899. The geological structure of the southern Malverns, and of the adjacent district to the west. Quart. Journ. Geol. Soc., lv, 129–169.Google Scholar
Harmer, F. W., 1928. The distribution of erratics and drift. Proc. Yorks. Geol. Soc., xxi, 79–150.CrossRefGoogle Scholar
Hey, R. W., 1958. High level gravels in and near the lower Severn valley. Geol. Mag., xcv, 161–8.Google Scholar
Pickering, R., 1957. The Pleistocene geology of the South Birmingham area. Quart. Journ. Geol. Soc., cxiii, 223–239.CrossRefGoogle Scholar
Richardson, L., 1935. Wells and springs of Herefordshire. Mem. Geol. Survey, England.Google Scholar
Shotton, F. W., 1953. The Pleistocene deposits of the area between Coventry, Rugby and Leamington and their bearing upon the topographic development of the Midlands. Phil. Trans. Roy. Soc., Ser. B 237, 209–260.Google Scholar
Symonds, W. S., 1907. The occurrence of oolitic remains in the gravels of Cradley, Herefordshire. Trans. Woolhope Nat. Field Club, 1852–1865, 48–50.Google Scholar
Symonds, W. S., and Lambert, A., 1861. On the sections of the Malvern and Ledbury tunnels (Worcester and Hereford Railway), and the intervening line of railroad. Quart. Journ. Geol. Soc., xvii, 152–160.CrossRefGoogle Scholar
Tomlinson, M. E., 1935. The superficial deposits of the country north of Stratford on Avon. Quart. Journ. Geol. Soc., xci, 423–462.Google Scholar
Wickham, W., 1899. On the drifts of our local rivers and brooks, with a short sketch of the sands in Mathon. Malvern Field Club, Malvern.Google Scholar
Wills, L. J., 1938. The Pleistocene development of the Severn from Bridgnorth to the sea. Quart. Journ. Geol. Soc., xciv, 161–242.Google Scholar