Clay-with-Flints
 | This article has multiple issues. Please help improve it or discuss these issues on the talk page. (Learn how and when to remove these template messages)
|
In geology, Clay-with-Flints was the name given by W. Whitaker in 1861 to a peculiar deposit of stiff red, brown or yellow clay containing unworn whole flints as well as angular shattered fragments, also with a variable admixture of rounded flint, quartz, quartzite and other pebbles.
Occurrence
The Formation is associated with deposits of the Chalk Group, subsequent Palaeogene and Neogene strata, and occasionally Upper Greensand.[1]
Formation
The formation is now considered to be a combination of residual and cryoturbated strata, and to be of a variety of ages.[2][3]
References
- ^ Cooper, Mark R.; Troll, Valentin R.; Lemon, Kirstin (November 2018). "The 'Clay-with-Flints' deposit in Northern Ireland: reassessment of the evidence for an early Paleocene ignimbrite". Geological Magazine. 155 (8): 1811–1820. Bibcode:2018GeoM..155.1811C. doi:10.1017/S0016756817000760. ISSN 0016-7568.
- ^ Anon. "Clay-with Flints formation". The BGS Lexicon of Named Rock Units. BGS. Retrieved 3 May 2017.
- ^ Gallois, R. W. (2009). "The origin of the Clay-with-flints: the missing link". Geoscience in South-West England. 12: 153–161.
External links
- Clay-with-Flints in the British Geological Survey lexicon.
This article incorporates text from a publication now in the public domain: Chisholm, Hugh, ed. (1911). "Clay-with-Flints". Encyclopædia Britannica (11th ed.). Cambridge University Press.
