CARBONIFEROUS DISTRICT OF PICTOU. 



:;_'.-. 



approximate to the original margin of the thick beds in this direction. 

 Such a place I should expect to find in the bend of the outcrop to 

 tlic westward of Mr Haliburton'a mine opposite New Glasgow. 



I have endeavoured to represent to the eye the above theoretical 

 views in the following ideal sections: — 



1 



s 



© 



a 



I 



•3 



I 



to 



S 



. a 



3 

 I 





to 



o 



►J 



C 

 3 



a 



I ° 



•a 



a 



c 

 .2 

 a 



s 





^ 



&5 



g 



J. 



5° 





3 



to 



CO 



to 



3 



H 



Cj 



3 

 o 

 O 



o 



w £3 



to 



•a 

 ■B 



l!' these views are correct, we have a right to expect that the tract 

 of Coal formation country to the northward of the great conglomerate, 

 ami extending from it to the eastern extremity of the Cumberland 

 district, should present characters similar to those of that district. 

 Accordingly the section on the tideway of the East River, and the 

 corresponding sections on the Middle River, and on the coast toward 



