| 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 [Obsolete Name and Code: Use CRRL]
(-2119)
|
| Alternative Name(s): |
none recorded or not applicable
|
| Stratotypes: |
| 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. |
| Reference(s): |
| Dean, M T, Browne, M A E, Waters, C N and Powell, J H. 2011. A lithostratigraphical framework for the Carboniferous successions of northern Great Britain (onshore). British Geological Survey Research Report, RR/10/007. 165pp. |
| 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 Unpublished PhD thesis, University of Lancaster.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 Airdrie district. Memoir of the British Geological Survey, Sheet 31W (Scotland). |
| 1:50K maps on which the lithostratigraphical unit is found, and map code used: |
|
S031
|
