36 
CLENT HILLS BRECCIA. 
similar to those exposed at the Lickey, but until the igneous rocks 
have been carefully examined and the question has been more care¬ 
fully considered as to what ridges lie concealed under the New Red 
Sandstone,* I think it is better to defer assigning, more definitely 
than I have, the exact source of origin. 
Another question, full of interest, is to what extent was the 
Bunter Pebble Bed derived from the aggregation of rocks forming 
the Permian Breccia. That there is similarity between the two 
is at once apparent. 
I cannot conclude without heartily thanking Dr. Lapworth for 
the great assistance he has given me from time to time. 
*On this, reference should be made to a paper by Mr. W. J. Harrison, 
Birmingham Philosophical Society’s Transactions, Yol. III., p. 157, on the 
Quartzite Pebbles contained in the Drift and in the Triassic Strata of 
England; and on their derivation from an ancient land barrier in central 
England. 
LIST OF FOSSILS. 
Description cf Fossil. 
Wych¬ 
bury. 
Clent. 
Walton. 
Roms- 
ley. 
Enville.j 
Quarry. 
Surface. 
Quarry. 
Surface. 
>> ' 
U 
o3 
3 
G> 
Surface. 
Quarry. 
Surface. 
Quarry. 
Surface. 
BltACHIOPODA. 
Atrypa Reticularis . 
X 
X 
X 
X 
Pentamerus sp . 
X 
,, galeatus ... 
X 
„ globosus ... 
X 
„ oblongus ... 
X 
X 
X 
X 
X 
,, rotundus ... 
X 
X 
,, undatus ... 
X 
Stricklandia lens . 
X 
X 
,, lirata . 
X 
X 
... 
... 
... 
... 
... 
... 
Rhynchonella sp . 
X 
,, borealis . 
X 
,, Llandoveriana 
X 
X 
,, nucula. 
X 
X 
• • • 
... 
... 
• *. 
X 
... 
X 
Orthis sp . 
X 
X 
,, biloba. 
X . 
,, caligramma. 
X 
X 
X 
• • * 
• •• 
... 
. • • 
X 
,, elegantula . 
X 
X 
X 
X 
• •• 
... 
... 
X 
... 
X 
„ hybrida. 
X 
X 
X 
... 
... 
... 
... 
... 
... 
X 
„ Menapiae? . 
X 
... 
... 
... 
... 
... 
„ patera . 
X 
,, testudinaria . 
X 
„ vesnertilio . 
X 
X 
X 
X 
... 
... 
... 
... 
... 
... 
Remarks. 
f Wychbury specimen 
t doubtful. 
Not given by Davidson 
as a Llandovery fossil, 
but all the others in 
same rock are. Com¬ 
pared it with every 
plate. 
f Clent quarry specimen 
t is an internal cast. 
February, 189B. 
