452 



ME. H. KAY ON THE HALESOWEN SANDSTONE [Oct. 1913, 



north by the flexure noted on p, 444. From the attenuated con- 

 dition of the blue clay seen in the new quarries at Hasbury (p. 445), 

 the beds of this group would appear to have been formed in a 

 shallow basin opening southwards. The necessary conditions would 

 be produced by a slight additional uplift of the buried anticline and 



Tig. 4. — Section from Wassel Grove to Oldenhall Colliery. 



S. , N. 



nw, 

 "Wassel Grove Hodge Hill 



Fig. 5. — Section from Oldenhall Colliery to Witley Colliery. 

 W. E. 



Oldenhall Beeches 



Colliery Colliery 



Witley 

 Lutley Brook Colliery 



[Scales: Horizontal, 3 inches = l mile; vertical, 1 inck=500 feet] 



the formation of the flexure already mentioned. This unconformity 

 also appears to be of purely local extent. 



The relations between the Keele Beds and the .Permian do not 

 come within the scope of this paper ; but I believe that unconform- 

 able relations will be found, as the various beds are traced from 

 south to north. 



