: 



division between llie Hunter Conglomerates and the Water-stones. It would appear 

 that the physical conditions under which the Conglomerates were deposited underwent 

 a slow and gradual change, the sediment merely becoming, as time went on, finer and 

 less pebbly in character. Throughout the area of the Leicestershire Coalfield there are 

 no indications to be met with of the unconformity between the Bunter and Keuper, 

 which appears to mark the" junction of these two divisions of the Trias in the neigh- 

 bourhood of Notlingham. 



B ^caU 3l'i.= OncMi2t 



KOTli.on.taL StcClJM. tVTJu^H- A B 



Geological Map of the Ingleby and Knowle Hill District, re-surveyed on the 

 six inch .scale, and reduceil one-half. 



