OBSERVATIONS ON THE NEW RED SERIES 
OF CUMBERLAND AND WESTMORLAND, WITH © 
ESPECIAL REFERENCE TO CLASSIFICATION. 
j (Read at the Penrith Annual Meeting of the Cumberland and Westmorland 
oe Association in Fune, 1892, and at the Edinburgh Meeting of the British ° 
‘ Association in August of the same year. ) 
By J. G. GOODCHILD, H.M. Grou. Survey, F.G.S., © 
Lecturer on Geology and Palzontology at the Heriot-Watt Collese 
Local Development. 
Discordance in Cumberland and Westmorland between the: Bunter 
Marts and the Strata below. 
Dyas or Lower New Red, and Permian, each used in a aleei 
SENSE, 
Paleontological Aspect of the Subject. 
General Hitstory of the New Red Series in Cumberland and West. 
morland. 
Changes of Subsequent Date. 
Some Papers on the New Red Series. 
‘Table of Lithological Characters and Thicknesses of the New Red 
Series in Cumberland and Westmorland. 
Figure 2, Comparative Sections of English New Red Series, 
H ( 1 UJ ok SPAS: or ; BetiCz 
5 F 
(Sete 
