THE GEOLOGY OF THE AREA AROUND LEINTWARDINE, HEREFORDSHIRE
- 1 March 1962
- journal article
- Published by Geological Society of London in Quarterly Journal of the Geological Society
- Vol. 118 (1-4), 319-347
- https://doi.org/10.1144/gsjgs.118.1.0319
Abstract
Wenlockian, Ludlovian, and lowest Downtonian strata have been mapped over an area of about ten square miles east of Leintwardine, where the structure is an asymmetrical syncline plunging east-north-east. The southern limb dips northward at about 35°, the northern limb eastward at about 8°.Keywords
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