LEGEND 



sfer 



Glacial drift ancl alluvivan. 



O 



i 



Kb 



Klslieiielui irormatioii. 



dijjefiy Jilirish.-ffrcy clctjys ; intcrl 

 oi* t^r&y .sfitn^f-St^n^ffosBUifer'atx 



r 



z 

 < 

 S 



00 



-i 

 o 

 o 



Entla, fomiatioxL 



inierhedaed. How or bdsi-^ lava. 



Steapai'd foramtioii. 



cMefiy thin.Ved^rd,,Vqht gfcy.mWjieouji 

 dolamijte>i an. ■mtcr'heiia.ei Hoyv afJiai-ic lav 



W''P 



Pu 





|_Gr 

 Gi-inixL-VL IftHTi 



■ chiefhf lh,n-hcridcd.r--l „i,-t,u-;,,Jlibi;<m 



Ap 



AppeliUiUTv fojtruuxoxi 



generally tMn-beMcd . hffh^ tjrcenuJi <p-e.y TnetaT-aiUite.. 



ALtvu fca^matioix 



tfiift-to t^tick-be^ided . hahiffrey, aenera/ZysoTufy.smcemis, 



Atve. dfAj'Ti ffr-i-y, 'f'rlspn.lhxsjed."(lolo-miix- 



Intrixsive 



Abnotciiial Gabliro 



Symbols 



Ge ological l)o-uiiSaiy 



R4°30' 



ocks, shown. Ails, 



BRITISH COLUMBIA <,S ALBjEBTA 



^^r:^H5?r3v ^ Great Plains 



--- Kyr" 



siticm of JLnnxs Tkmist 



CRETACEOUS 



Sections alojig liD_e AA'BCDEF 



GEOLOGY OF THE FORTY-NINTH PARALLEL, BjR.A.Daly. 



Scale: 62500 = 09864 Statute Miles to llnck 



IReprtntfed^ by permzsstoTh of Chief AstnonoTner, 

 to cuxomparvy Geologiaai Survey Memoir 2^938 



CoTitowr intervaL, 100 feet 



