GEOLOGICAL NOTES—BURTON-ON-TRENT. 24 
Tatenhill cliff—another good example on the other side of the 
valley—and the section, now rapidly becoming overgrown, below the 
Reservoir, are also good examples of the Red Marl Beds of the 
Upper Keuper. 
Fav.ts. 
T had always understood that there were two, if not three, distinct 
Faults crossing the Bearwood Hill, but Mr. Adrian Brown and I 
have only been able to prove the presence of one, and that a most 
obvious one. Mr. Fox Strangways also only mentivns one in his 
paper before referred to. 
It is toward the top of the hill, and the massive dark-coloured 
bed of tough Carbonaceous sandstone ends abruptly on either side 
