Hostname: page-component-cd9895bd7-mkpzs Total loading time: 0 Render date: 2024-12-26T16:19:16.359Z Has data issue: false hasContentIssue false

III.—On the Occurrence of Grey-Wethers at Grays, Essex

Published online by Cambridge University Press:  01 May 2009

Extract

The occurrence of “Sarsen-stones,” or blocks of so-called Druid sandstone, has not, I believe, been generally noticed in this locality, and their position may be of interest to some of your readers, more especially as the extensive working both for Brick-earth and Chalk have obliterated many of the interesting sections for which the pits were celebrated. Grays is well known both for its fine chalk-pits and extensive brick-earth deposits, the latter containing numerous remians of fossil mammalia, associated with land and fresh water mollusca. The sarsen-stones (of which some may be still seen lying about the large chalk-pit), I have noticed during the progress of the workings as occurring on the upper surface of a bed of disturbed chalk, above the solid chalk, and covered by a blackish or carbonaceous clay containing freshwater shells.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1867

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

1 Mag. Nat. Hist. 1836, p. 261Google Scholar; 1838, p. 539.Google Scholar