ADDENDA AND CORRIGENDA. 



Page. 





Line, 



for 



read 



30 





27 



living shale 



living shell 



44 





22 



Dark 



Park 



53 





32 



Plate I. 



Plate IV. 



60, note 



* 



1 



seen 



won 



63 





16 



eastern edge 



western edge 



68 





10 



more 



mere 



71, note 



* last line 



•• 



Plate VII. fig. 3 

 Plate V. fio-, 1 



Plate VII. fig. 1 



Plate V. fig. 3 



Mill on the River 



88 





27 



Mill or River 



108 





24 



remains at Cold Hill 



remains. At Cold Hill 







25 



Aberford : in a few 



Aberford and in a few 



110 





20 



and in the descending 



and is in the descending 



110, note 



u 





p. 110 



p. 93 



. . ., note 



tt 



1 



five species of Melaniae 



a species of Melania 



129 





27 



Forhabres 



Fochabres 



134, note 





2 



medicinal 



economical and medicinal 



135 





26 



Gornigo 



Gernigo 



14.1 





2 



bed 



beds 



157 





g 



country. They are 



country they are 



303 

 305 





24/ 



primary or transition 



primary and transition 



312 





4 



of a large 



of large 



312 





20 ] 



By the expressions here used, 



the authors do not intend 



388 



13 



394 



25 



403, note. 





413 



18 



424 

 424, note 



24 



to convey the idea of any general analogy between the 

 fossils of the rock in question, and those of the moun- 

 tain limestone. / 



scalarm ? Scalaria ? 



Graub-kalk Grob-kalk 



In addition to M. Constant Prevost also M. P. Partsch 



The eastern extremity of the chain, &c. In limitation 



of the assertion in this paragraph, we may state that 



the younger tertiary conglomerates and Leitha-kalk 



of WoUersdorf are considerably inclined. We believe, 



however, that the cases of this kind are exceptions 



which do not affect the general rule. 



formation of the same age nearly of the same age 



2 from bottom, Cullompton 



Cullumpton 



