Computer Code: |
NWE |
Preferred Map Code: |
notEntered |
Status Code: |
Full |
Age range: |
Dimlington Stadial (QDD)
— Dimlington Stadial (QDD) |
Lithological Description: |
Comprises up to 20 m or more of sand and gravel forming a beaded ridge that extends discontinuously for about 55 km in a north-north-west - south-south-east direction from the Thirsk area in the north to Aldwark in the south. At its southern end it terminates as a delta deposit in the Alne pro-glacial lake. South of this the Poppleton Glaciofluvial Member and the Crockey Hill Esker Member both have the same orientation and may be related as precursor deposits when the ice-front was further south (Powell et al., 1992; Cooper and Burgess, 1993).
Late Devensian, Dimlington Stadial (MIS 2). |
Definition of Lower Boundary: |
none recorded or not applicable
|
Definition of Upper Boundary: |
none recorded or not applicable
|
Thickness: |
Up to 20 m or more. |
Geographical Limits: |
Vale of York. |
Parent Unit: |
Vale Of York Formation (VYORK)
|
Previous Name(s): |
none recorded or not applicable
|
Alternative Name(s): |
none recorded or not applicable
|
Stratotypes: |
none recorded or not applicable |
Reference(s): |
McMillan, A A, Hamblin, R J O, and Merritt, J W. 2011. A lithostratigraphical framework for onshore Quaternary and Neogene (Tertiary) superficial deposits of Great Britain and the Isle of Man. British Geological Survey Research Report, RR/10/03. 343pp. |
Powell, J H, Cooper, A H C and Benfield, A C. 1992. Geology of the country around Thirsk. Memoir of the British Geological Survey, Sheet 52 (England and Wales). |
Cooper, A H and Burgess, I C. 1993. Geology of the country around Harrogate. Memoir for 1:50000 geological sheet 62 (England and Wales). London: HMSO for the British Geological Survey. |
1:50K maps on which the lithostratigraphical unit is found, and map code used: |
none recorded or not applicable |