



<4 



.2-t-> 



® d 



e lower 

 in the 

 tin foot 

 he Kerr 

 n hang- 







Eh 

 < 



r— ^ 

 CO 



O d 



£ bcco-^iJ 

 C £ e! £? 



.S'SSo^ 







ffl 

 O 



u 



H 



M 



H 



03 



H CD 



CO »—< 



alt series, : 

 the Nipis 

 in the K« 

 as No. 3 

 in the Kee 



U) 



u 



E 





O 



P? 

 < 



Ph 



CD 



*£ 



cd Eh 



1 rocks, Cob; 



No. 26 on 



erson lake, 



itself, such 



properties, 



UJ 





> 



J3 



CO W+? (h 



■H cd <?> -h cd 



< 





U 



P 

 Q 

 O 



O a 

 -t-> 



I-H CD 



3 » 



f ragmen 

 , such 

 under F 

 the sil 

 or Beav 



CD 





Cm 



HI CD 



c c 



5>gcS 



O 



'53 



cc5-t-> 



o 



> 



H 



5 



•5 5 



• rt o to f> CO 



T7"] 



H 



S' rt 



CD d .M 







>d 



r, CD CO to 





'•5 







ho © 



tj ft ,3 "2 







.S o 



£* 



o 



P 

 O 

 Ph 



C0+-> 



72 s 



.Cd^.-EH-- 





ft 



•H CD 



veins t 

 esents 



a type 

 the sill 

 on the 



the sil 





S 



M 



B w 







Eh 



CD 

 J2 CD 







O 



■<-> CD 



shows it to be. 

 represent a large number of 

 1 of the eroded sill. N repr 

 elow the eroded sill, and L 

 ot extending upward into i 

 ty; T, a vein such as that 

 d extending downward into 







rn 



o E 



z 



to 

 c 

 'S 

 > 



EH 

 U 



H 

 oa 



< 

 o 



Eh 



.2* 



COr^ 



CD 

 JS CD 



< 



u 



UJ 





Fh 

 !> 



Q 



H 



to Eh 



,-,'cD 



* 





3 



CD i 

 CD O 



ustration 

 B and C 

 ■ foot wal 

 eewatin b 

 all, but n 

 ke proper 

 g wall an 



2 











■o 



CO 



3 oW£5.S 



