Abstract
The series of estuarine deposits which occurs at Kirmington, North Lincolnshire, situated between Brown Boulder Clay and Purple Boulder Clay, has long been recognized as of considerable importance owing to its inter-glacial position. The best description of the complete sequence of beds overlying the Chalk at this locality has been afforded by a Committee of the British Association (1).
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: 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.