The BGS Lexicon of Named Rock Units — Result Details

Corrie Lava Member

Computer Code: CRRL Preferred Map Code: notEntered
Status Code: Full
Age range: Arundian Substage (CJ) — Asbian Substage (CR)
Lithological Description: The Corrie Lava Member consists of plagioclase-macrophyric basalt and trachybasalt lavas (of 'Markle' type), aphyric basaltic-trachandesite (mugearite) lavas, and lapilli-tuff and tuff-breccia beds. Derivation is thought to be from local vents (Craig, 1980).
Definition of Lower Boundary: The Corrie Lava Member is fault-bounded and the lower boundary is not seen.
Definition of Upper Boundary: The Corrie Lava Member is fault-bounded and the upper boundary is not seen.
Thickness: More than 30 m, neither lower or upper boundaries are seen
Geographical Limits: The member is restricted to the southern part of the Campsie Block and specifically to the southern side of the south-western Kilsyth Hills, north of Glasgow. The outcrop is bounded to the south by the Campsie Fault, to the north by the Bachille Fault and to the north-east by the East Bachille Fault.
Parent Unit: Clyde Plateau Volcanic Formation (CPV)
Previous Name(s): Corrie Lavas (-2119)
Alternative Name(s): none recorded or not applicable
Type Area  South-western Kilsyth Hills, north of Glasgow Forsyth et al, 1996, after Craig, 1980 
Reference Section  Unnamed burn crossing escapment north of Corrie, south-western Kilsyth Hills, north-east of Glasgow Craig, 1980 
Craig, P.M. 1980 The Volcanic Geology of the Campsie Fells area, Stirlingshire. Unpublished PhD thesis, University of Lancaster. 
Forsyth, I H, Hall, I H S and McMillan, A A. 1996. Geology of the Aidrie district. Memoir of the British Geological Survey, Sheet 31W (Scotland). 
1:50K maps on which the lithostratigraphical unit is found, and map code used: