376 



DR. ^\. HIND AND MK. J. A. HOWE ON THE [Aug. IQOI, 



the country between Pendle Hill and Castleton, but north, south, 

 and west of these points the beds rapidly thin out. 



In lithological and palaeontological characters these beds are 



Fig. 1. 



LOCALITIES. 



1 CLITHERO.E & PENDLE HILL 



2 SKIPTON 



3 LONGRTD.GE 



4 MARSDEN 



5 LEEK 



6 CkSJinO^ CPeak DJstrlcif- 



7 MATLOCK 



8 ASHBOURNE 



9 LEYBURN 



10 POOLVASH (Isle of Man) 



11 DUBLIN 



12 FOYNES ISLAND 



13 VENN 



14 BUDLE 



Land _„, . 



Pendleside Gmxrp. 



Sketch-Map of the 

 BRITISH ISLES 



to indicate the ar.ea occupfed by 

 the 



PENDLESIDE 

 GEOUP. 



entirely different from the Yoredale Series of Wensleydale, and are 

 altogether above it, for the strongest palaeontological and strati- 

 graphical evidence shows that the Yoredale Series of Wensleydale 

 is the homotaxial equivalent of the upper portion of the Carboni- 

 ferous Limestone massif. 



