Abstract

THE current reconstruction of the Devensian Till stratigraphy of Holderness1 invokes three units—the Drab, Purple and Hessle Tills—with the Hessle overlapping both lower tills so as to be the only one present in the westernmost part of the area, on the Yorkshire Wolds. Because of the characteristic reddish brown colours (usually 5YR4/4 of the Munsell Soil Colour Charts, 1954) of the uppermost tills throughout eastern England, the upper till in Lincolnshire and the Hunstanton Till of north Norfolk are equated usually with the Hessle Till1–5, although Straw6 correlated his two Marsh Tills in Lincolnshire with the Drab and Purple Tills of Holderness, and Bisat7 equated the Hessle Till of the Yorkshire Wolds with his Middle Drab division.

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 call

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.