Annual report . ?• ;/ .. ..%&: > *&**.. \\K. 66- Schistose conglomerate of Temiskaminj* series, Lake Savant area. LiteratureLake Savant [roil Range Area, by E. S. Moore, 19th Report, Bureau of Mines, Ontario,pp. 173-193. Vermilion Lake Ivrite I><-posits, liv 10. S. Moore, 20th Report, Bureau of Mines, Ontario,Part I, pp. 199-213. 14. STEEP ROCK LAKE From the descriptions of this area the writers consider that the Temiskamingseries is present. One series, consisting of conglomerate and fossiliferous limestonewhich rest unconformably on the Keewatin and Laurentian, is known as the Steep
Annual report . ?• ;/ .. ..%&: > *&**.. \\K. 66- Schistose conglomerate of Temiskaminj* series, Lake Savant area. LiteratureLake Savant [roil Range Area, by E. S. Moore, 19th Report, Bureau of Mines, Ontario,pp. 173-193. Vermilion Lake Ivrite I><-posits, liv 10. S. Moore, 20th Report, Bureau of Mines, Ontario,Part I, pp. 199-213. 14. STEEP ROCK LAKE From the descriptions of this area the writers consider that the Temiskamingseries is present. One series, consisting of conglomerate and fossiliferous limestonewhich rest unconformably on the Keewatin and Laurentian, is known as the Steep Rock. In addition to the Steep Rock series there is a series of conglomerates and otherrocks which Lawson has named the Seine series and of which the Shoal Lake conglomer- *A Geological Reconnaissance of the Region Traversed bv the Nat. Trans. Ry. betweenLake Nipigon and Clay Lake, Ont., Rep. Geo!. Sur. Canada, 1909, p. 34. 1913 Appendix 137 ate forms a part. Lawson believes that the Seine sh rdes lii s unconformably on the SteepRock ser
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