FAULTING 



365 



between Rockland and Hollins, two stations on the Northern Central 

 railroad, shows in detail the complexity of the structure in this area as 

 well as the observations on which the present interpretation is based. 



SECTION ALONG LINE AB 



SECTION ALONG LINE CD. 



e 



o 



xv^xn^^ffftS^.- ■ 



t.A 



v \ v \ x V ». ^O/T-VfVT A -V-* , X 



t-t»»L 



\\\ w\.^" «-Cii-Tj-'LJ< °. V X. 





\v\\w-<^<. ^ • • *^sJ>. 





LEGEND. 



V * 



SER PCNTINC, 



WISJAHK KON 

 SCHIST, 



CI? Y5 TALLIHZ 

 Ll ME STOW ET. 



SETTER'S 



Quartz /re 



BALTIHCRE 

 G-NElSS. 



m 



FAULT 



u n e. 

 ^ — 



SECTION 

 L/NF. 



Dip AND 

 STRIKE. 



S CA L£ 



MILE. 



Figure 2.— Map af Vicinity of Rockland. 



On the west is the eastern end of the southwestern anticlinal dome already 

 described, and on the east the southerly extension of the fault under dis- 

 cussion. Earlier work in the region led Doctor Williams to interpret the 



