The BGS Lexicon of Named Rock Units — Result Details

Beinn an Uain Till Formation

Computer Code: BUTI Preferred Map Code: BAU
Status Code: Full
Age range: Devensian Stage (QD) — Devensian Stage (QD)
Lithological Description: Stoney sandy clay diamicton, matrix-supported, dark yellowish brown to olive-grey, fissile, massive, extremely compact, containing angular to subrounded clasts of gneissose psammite and semipelite, granite and some Devonian sandstone and siltstone. Typical lodgement till with well developed north-easterly fabric and containing concavo-convex discontinuities that are commonly sand-filled.
Definition of Lower Boundary: Generally a gradational contact over 10-20cm, or locally a sharp, planar one, with stony, sandy diamictons of the underlying Athais Till Formation, or on bedrock.
Definition of Upper Boundary: Erosional contact with gravel of the Carn Monadh Gravel Formation at the Allt Odhar Interstadial site, various younger deposits or the ground surface.
Thickness: 10m
Geographical Limits: Sheet 84W (Fortrose), southeast of Inverness.
Parent Unit: Central Grampian Glacigenic Subgroup (CGDR)
Previous Name(s): The Moy Upper Till Member [Obsolete Name and Code: Use BUTI] (-4506)
The Dalcharn Upper Till Formation (-737)
Alternative Name(s): none recorded or not applicable
Stratotypes:
Partial Type Section  Exposed at the top of river cliffs of the Allt Odhar, immediately upstream of its confluence with the Caochan nan Suidheig, Moy Estate, 16km southeast of Inverness Walker, M J C and 6 others. 1992. 
Partial Type Section  River cliff sections of the Allt Dearg, 6km southwest of Cawdor, Nairnshire. The Dalcharn Interglacial site Walker, M J C, and 6 others. 1992. 
Reference(s):
Fletcher, T P et al. 1996. Geology of the Fortrose and eastern Inverness district. Memoir of the British Geological Survey, Sheet 84W (Scotland). 
Walker, M J and 6 others. 1992. Allt Odhar and Dalcharn: two pre-Late Devensian (Late Weichselian) sites in northern Scotland. Journal of the Quaternary Science, Vol.7, 69-86. 
Sutherland D G and Gordon, J E. (editors). 1993. The Quaternary of Scotland. Geological Conservation Review Series: 6. London: Chapman and Hall. 
1:50K maps on which the lithostratigraphical unit is found, and map code used:
S084