Abstract
The Lower Old Red Sandstone sequence in the area of the Cleobury Mortimer syncline is closely comparable with that in Corvedale. The ‘Holdgate Sandstones’ are recognised and it is shown that individual ‘ Psammosteus’ Limestones can locally be more accurately mapped by geophysical (resistivity) methods. White's ostracoderm zones are recognised and the unfossiliferous Breconian Clee Series is probably present. No Upper Old Red Sandstone has been detected. The relationship of the syncline to the structure of the Clee Hills is briefly considered.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
