124 



C. Edmnonds — 



*Lonsdaleia floriformis laticlavia 



S. Smith. 

 Productus giganteus Mart., var. 

 Productus latissimus J. Sow. 

 P. pugilis Phill. 



* Not known at other horizons 



niut. pachyendothecum 

 S. Smith. 



West Cumberland 

 L "Tie stones 



Okton Moor Series. 



l^llUtme &„f , 



Lime.s1orie\ 



SeconJ j 

 LimesTcne. \ 





-tic ^\> PIS ■ 



gffift5.^>4^.^^^ 



5 SmiTJi- 



Great Limestone, 



Sandstone i Shale. 

 Litlle. Li^nefctone. 



Quai-r). Hazel. 



roui- ra»lKom LimesTpue: 



Three Ycxxd. 



Five wa. .. 



Coi.k\c Sliell 



Tvne. .Bottortx. ,, 

 Jpw- Llmc'torie, 



RobinbOnb LirnebtcnC. 



Fig. 2. — Faunal Comparison of the Limestones of West Cumberland with those of the 



Alston Moor District. 



Besides the similarity of their fauna both limestones have a lower 

 massive portion and an upper more thinly-bedded one, in which 

 bedding j)lanes and partings of thin shales are very sinuous but 

 remarkably persistent, individual beds being recognizable at places 

 as far as 10 miles apart. An examination of the beds of the Great 

 Limestone of a district so far removed from our area as Fourstones 



