The BGS Lexicon of Named Rock Units — Result Details

Eagle Moor Sand and Gravel Member

Computer Code: EMSG Preferred Map Code: symb
Status Code: Full
Age range: Mid Pleistocene (QPM) — Mid Pleistocene (QPM)
Lithological Description: Predominantly cold-phase sands and gravels that underlie the Eagle Moor Terrace. Dominated by rounded pebbles of "Bunter" quartz/quartzite with subordinate subangular flint (typically 25% in the Type Area), etc. Clayey and poorly sorted. In type area occurs as hill-top outliers falling from c.36m OD near Newark (c.25m above Trent floodplain) towards the Lincoln Gap, being at c.+32m OD at Eagle Moor and possibly descending more rapidly to the east. Outliers upstream in the Loughborough district 30m+ above Trent floodplain. Correlated with the Martin Sand and Gravel Member (Trent Valley Formation), east of the Lincoln Gap. River terrace deposits. Middle Pleistocene (MI Stage 12 or 10).
Definition of Lower Boundary: Unconformable, commonly channelled base, resting on pre-Quaternary bedrock or locally, east of Eagle Moor, on the Skellingthorpe Clay Member of the Wolston Formation.
Definition of Upper Boundary: Ground surface.
Thickness: 0 to c. 6 m; typically c. 2 to 3 m.
Geographical Limits: Newark on Trent to Lincoln Gap (British Geological Survey sheets 113, 114, 126, 126; see Brandon and Sumbler, 1991, Figure 1) with probable outliers upstream in the Uttoxeter-Derby area (sheets 140, 141; included in Trent, Trent-Derwent and Soar Valley formations) and possibly elsewhere.
Parent Unit: Trent Valley Formation (TRVA)
Previous Name(s): Older river sand and gravel (ORSG)
Eagle Moor Member [Obsolete Name and Code: Use EMSG] (-3387)
Glacial sand and gravel [Obsolete Name and Code] (GSG)
Hilton Terrace Deposits [Obsolete Name and Code: Use EMSG] (-2172)
Older river sand and gravel (ORSG)
Eagle Moor Sand and Gravel [Obsolete Name and Code: Use EMSG] (-233)
Upper Hilton Terrace (in part) [Obsolete Name and Code: Use EMSG] (-234)
Alternative Name(s): none recorded or not applicable
Stratotypes:
Type Area  Eagle Moor. Brandon and Sumbler, 1988; 1991; Berridge et al., 1999. 
Reference(s):
Stoker, M S, McMillan, A A and Waters, C N. Quaternary Stratigraphical Chart: Southern Britain. British Geological Survey, 1 poster. 
Carney, J N, Ambrose, K and Brandon, A. 2002. Geology of the Loughborough district. Sheet explanation of the British Geological Survey, Sheet 141 (England and Wales). 
Brandon, A, and Sumbler, M G. 1988. An Ipswichian fluvial deposit at Fulbeck, Lincolnshire and the chronology of the Trent terraces. Journal of Quaternary Science, Vol. 3, 127-133. 
Clayton, K M. 1957. Differentation of the glacial drifts of the East Midlands. East Midlands Geographer, Vol.1, 31-40. 
Gozzard, J R. 1976. The sand and gravel resources of the country east of Newark upon Trent, Nottinghamshire: description of 1:25 000 resource sheet SK86 and part of SK76. Mineral Assessment Report, Institute of Geological Sciences, No.20. 
Howard, A J. 1992. The Quaternary Geology and geomorphology of the area between Newark and Lincoln. Unpublished PhD Thesis, University of Derby. 
Pocock, T I. 1929, The Trent valley in the glacial period. Zeitschrift fur Gletscherkunde, Vol.17. 302-318. 
Straw, A. 1963. The Quaternary evolution of the lower and middle Trent. East Midlands Geographer, Vol.3, 171-189. 
Straw A and Clayton, K M. 1979. The Geomorphology of the British Isles: Eastern and Central England. (London: Methuen). 
Berridge, N G, Pattison, J, Samuel, M D A, Brandon, A, Howard, A S, Pharaoh, T C, and Riley, N J. 1999. Geology of the Grantham district. Memoir of the British Geological Survey, sheet 127 (England and Wales). 
Clayton, K M. 1953. The glacial chronology of part of the middle Trent basin. Proceedings of the Geologists' Association, Vol.64. 198-207. 
Edwards, W N, 1967. Geology of the country around Ollerton (2nd edition). Memoir of the Geological Survey of Great Britain, sheet 113 (England and Wales). 
Jackson, I. 1977. The sand and gravel resources of the country west and south of Lincoln, Lincolnshire: description of 1:25 000 resource sheets SK95 and part of SK96 and SK97. Mineral Assessment Report, Institute of Geological Sciences, No.27. 
Bowen, D Q. 1999. A revised correlation of Quaternary deposits in the British Isles. Geological Society Special Report, No. 23. 
Swinnerton, H H. 1937. The problem of the Lincoln Gap. Transactions of the Lincolnshire Naturalists' Union, Vol.9, 145-153. 
Brandon A, and Sumbler, M G. 1991. The Balderton Sand and Gravel: pre-Ipswichian cold stage fluvial deposits near Lincoln, England. Journal of Quaternary Science, Vol. 6. 117-138. 
1:50K maps on which the lithostratigraphical unit is found, and map code used:
E126 E127 E141 E113 E114 E140