402 DE. W. FIND AND MR. J. A. HOWE ON THE [Aug. I9OI, 



Craven with that of the Yoredale Series of Northern Yorkshire ; and 

 thirdly, the true position of the inliers of Ashnot, Bolland, Cracoe, 

 and Thorpe in Craven. The lists do not in any way profess to be 

 complete. 



The corals, gasteropoda, and crustaceans have not been included, 

 as the necessary details have not yet been obtained with sufficient 

 accuracy for publication ; but even now it is certain that the dis- 

 tribution of the corals, which are plentiful in the limestones of the 

 Yoredale Series, will demonstrate the identity of the faunas in 

 the Yoredale and Massive Limestones. The few gasteropods as yet 

 obtained in the Pendleside fauna are, however, noted, and only a 

 single coral (Zajohrentis Enniskilleni) has been recorded from this 

 horizon . 



In conclusion we wish to express our sincere thanks for the help 

 most generously afforded to us by Dr. G. J. Hinde, F.R.S., Dr. Henry 

 "Woodward, F.It.S., Mr. George C. Crick, aud Dr. A. H. Foord in the 

 determination of specimens. 



PLATE XIV. 



Comparative vertical sections of the Pendleside Grroup, on the scale of 



80 feet to the inch. 



Discussion. 



Mr. Make bore testimony to the value of the work which Dr. Hind 

 was carrying out with such enthusiasm. He was much impressed, 

 when in the field with Dr. Hind, by the way in which that worker 

 had predicted the occurrence of the Pendleside fauna in certain beds 

 near Ciacoe, and had then found them. But he (the speaker) 

 would like more information concerning the faunas below this. 

 Dr. Hind maintained that the great group of ' shales with lime- 

 stones,' which had by other workers been intercalated between two 

 sets of limestone, came above the Pendleside Limestone, and that 

 the beds between the base of the Great Scar Limestone and the 

 Upper Scar Limestone lying north of the Craven Pault were all 

 represented by limestone to the south of that fault. He (the 

 speaker) felt that this question could only be satisfactorily settled 

 by working out in detail the faunas of the limestones and shales to 

 the north of the Craven Pault ; this he believed had never yet been 

 satisfactorily accomplished, and if the Authors had not done it in 

 the paper of which they had necessarily given only a brief abstract, 

 he hoped that it would be done ere long. 



Prof. Garwood congratulated the Authors on the results of their 

 careful work in the Pendleside Limestone Group. He could not, 

 however, quite follow the evidence of the fluviomarine origin of the 

 beds. With regard to Dr. Hind's classification of the whole of the 

 Mountain Limestone and Yoredale Series as the zone of Productu§ 



I 



