SECTIONS m WARWICKSHIRE. 275 



Rhaetic ; he asked if the Ehaetic beds seen in the shafts could 

 possibly have slipped down from the elevations in the neighbourhood, 

 or whether there was any chance of the Rhsetics being transported 

 masses in drift. 



The Author said the Snitterfield section was drawn below the 

 surface by a very good engineer and geologist, but he had not him- 

 self been able to examine all the details. He saw no reason for 

 believing that the beds were not in place, but he could not speak 

 quite positively. In reply to Mr. Ussher the Author observed that 

 the sun-bed (limestone) did not occur in Warwickshire, and was 

 confined to Somersetshire. 



