30 



tion well illustrates the type of lake scenery to be found 

 in the Keweenanwan and Animikie rocks. Occasionally 

 taconite, along with the Animikie slate, is found overlying 

 the sill. A magnificent view of Thunder bay and Thunder 

 cape can be seen from one of the more open spots a little 

 farther along. In descending from this last point to the 

 valley the contact of the sill with the underlying Animikie 

 slates is passed. To the north is another exposure of 

 taconite upon which some prospecting has been done. 

 One mile west of the railway station, in a railway cut, is 

 a remarkable conglomerate intersected by two small 

 dykes apparently connected with the Logan sills. 



BIBLIOGRAPHY. 



1. Logan, W. E Rep. of Progress, G.S.C. 1846-7, 



pp. 1-46. 

 2 Geology of Canada, Rep. of Progress. 



G.S.C. 1863, pp. 67-86. 



3. Rep. of Progress, G.S.C. 1863, 



A f-loc 



4. Bell, R Rep. of Progress, G.S.C, 1866-69, 



PP- 3I3-364- 



5. Ingall, E. D Ann. Rep. G.S.C. (New Series) Vol. 



Ill, Pt. F. 



6. Smith, W, N Ont. Bur. Mines, Vol. XIV, 1905, 



Pt. I, pp. 254-260. 



7 Mining World, Vol. XXII, 1905, 



pp. 206-208. 



8. Silver, L.P Ont. Bur. Mines, Vol. XVI, 1905, 



Pt. I, p. 156-172. 



9. International Committee on Pre-Cambrian Nomencla- 



ture. Jour. Geol. Feb. -Mar. 1905, 



ANNOTATED GUIDE— (Continued). 



Miles and 



Kilometres One mile (1 • 6 km.) west of Loon a remarkable 



from Sudbury- i . • i • -i 



* conglomerate is exposed in a railway cut. 

 From this point to Port Arthur the rock is 

 of diversified character, including Laurentian, 

 Keewatin, Animikie and Keweenawan, with 

 no very striking exposures of any of them. 

 554 m. Port Arthur. — Altitude 608 ft. (189-3 m -)- 

 891 -5 km. 



