58 THE DAWN OF LIFE. 



limestone, occasionally interstratified with diorites, and 

 near the base with silicions slates and small beds of 



impure steatite 330 



This limestone, which is often silicions and ferrugin- 

 ous, is metalliferous, holding disseminated copper 

 pyrites, blende, mispickel, and iron' pyrites, the latter 

 also sometimes in beds of two or three feet. Gold occurs 

 in the limestone at the village of Madoc, associated with 

 an argentiferous gray copper ore, and in irregular veins 

 with bitter-spar, quartz, and a carbonaceous ma^tter, at 

 the Richardson mine in Madoc. 



6. Gray silicious or fined-grained mica-slates, with 

 an interstratified mass of about sixty feet of yellowish- 

 white dolomite divided into beds- by thin layers of the 

 mica-slate, which, as well as the dolomite, often becomes 

 conglomerate, including rounded masses of gneiss and 

 quartzite from one to twelve inches in diameter 400 



7. Bluish and grayish micaceous slate, interstratified 

 with layers of gneiss, and' occasionally holding crystals 

 of magnetite. The whole division weathers to a rusty- 

 brown _ ..._..... 500 



8. Gneissoid micaceous quartzites, banded gray and 

 white, with a few instratified beds of silicious lime- 

 stone, and, like the last division, weathering rusty 

 brown 1,900 



9. Gray micaceous limestone, sometimes plumbagin- 

 ous, becoming on its upper portion a calc-schist, but 

 more massive towards the base, where it is interstratified 

 with occasional layers af diorite, and layers of a rusty- 

 weathering gneiss like 8 1,100 



This division in Tudor is traversed by numerous 

 K.W. and S.E. veins, holding galena in a gangue of 

 calcite and barytine. The Eozoon from Tudor here 

 described was obtained from about the middle of this 

 calcareous division, which appears to form the summit 



of the Hastings series. 



Total thickness 21,130 



