XXVII.—The Forest of Wyre and the Titterstone Clee Hill Coal Fields.
Open Access
- 1 January 1917
- journal article
- research article
- Published by Cambridge University Press (CUP) in Transactions of the Royal Society of Edinburgh
- Vol. 51 (4) , 999-1084
- https://doi.org/10.1017/s0080456800011960
Abstract
The investigations recorded in this communication were begun some years ago, and arose chiefly as the result of two papers published on the Geology of the Forest of Wyre by Mr T. C. Cantrill, B.Sc.In the latter paper Mr Cantrill, after carefully summarising all the available data respecting the age of the so-called “Permian” of the Forest of Wyre (= Enville), arrives at the following conclusions:—I. That these “Permian” rocks are of the same age as those at Hamstead in South Staffordshire.II. That the Hamstead red rocks were shown by their flora to be Upper Coal Measures.Keywords
This publication has 2 references indexed in Scilit:
- On the Fossil Flora of the Pembrokeshire Portion of the South Wales CoalfieldQuarterly Journal of the Geological Society, 1913
- Die Oberschlesische Steinkohlenflora. I. Teil, Farne und farnähnliche Gewächse (Cycadofilices besw. Pteridospermen)Published by Biodiversity Heritage Library ,1913