The BGS Lexicon of Named Rock Units — Result Details

Close Hill Siltstone

Computer Code: CLHS Preferred Map Code: ClHS
Status Code: Full
Age range: Arnsbergian Substage (CG) — Arnsbergian Substage (CG)
Lithological Description: Siltstone, grey, sandy, micaceous, calcareous with rhythmic layers of fine-grained red-brown weathering, sandstone to 1cm; sporadic to common layers of sandy calcisiltite; rare to common Sanguinolites and bellerophontids. NOTE: This is a distinct/unique lithology within the Roeburndale Formation. The formation consists of delta slope siltstones with sandstones. There were previously three known marine bands with goniatite/bivalve faunas. The Close Hill Siltstone is a fourth new marine band.
Definition of Lower Boundary: Gradational to grey planty siltstones with common planty micaceous fine- to medium-grained sandstones over 10cm. (Delta slope deposits).
Definition of Upper Boundary: As lower boundary.
Thickness: c. 60m
Geographical Limits: Not known; probably extensive. Known from large area of Lancaster Fells, and probably extends throughout Lancaster Sheet.
Parent Unit: Roeburndale Member (RBL)
Previous Name(s): Close Hill Siltstone Member [Obsolete Name and Code: Use CLHS] (-4551)
Alternative Name(s): none recorded or not applicable
Stratotypes:
Reference Section  Wray Borehole, 220-280m depth. 
Reference Section  Hamstone Gill. (top c.16m only well exposed). 
Type Section  Raghill Beck, near Close Hill. Bed of stream and meander scarps along Raghill Beck. 
Reference(s):
Waters, C N, Waters, R A, Barclay, W J, and Davies, J R. 2009. Lithostratigraphical framework for Carboniferous successions of Southern Great Britain (Onshore). British Geological Survey Research Report, RR/09/01. 184pp. 
Brandon, A, Aitkenhead, N, Crofts, R G, Ellison, R A, Evans, D J, and Riley, N J. 1998. Geology of the country around Lancaster. Memoir of the British Geological Survey, Sheet 59 (England and Wales). 
Slinger, F C, 1936. Millstone Grit and glacial geology of Caton Moor near Lancaster. Report of the British Association for the Advancement of Science, Blackpool 1936, 345. 
1:50K maps on which the lithostratigraphical unit is found, and map code used:
E059