The BGS Lexicon of Named Rock Units — Result Details

Newby Wiske - Aldwark Esker Member

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