AND KAKLV I'AL.KOZOIC. \* 



We may compare the disseminated graphite to ilia! 

 which we find in (hose districts of Canada in which Silu- 

 rian and Devonian hituminous shales and limestones have 

 heen metamorphosed and converted into graphitic rocks 

 not very dissimilar to those in the less altered portions of 

 the Laurent ian.* In like manner it seems prohahle that 

 the numerous reticulating veins of graphite may have 

 heen formed by the segregation of bituminOUB matter into 

 .iiivs and planes of least resistance, in the manner in 



ich such veins occur in modern bituminous limestones 

 id shales. Such bituminous veins occur in the Lower 

 Carboniferous limestone and shale of Dorchester and 

 Hillsborough, New I Brunswick, with an arrangement very 

 similar to that, of the veins of graphite ; and in the Que- 

 bec rocks of Point, Lex i, veins attaining to a thickness of 

 more t ban a foot, are filled with a coaly matter having a 

 transverse columnar structure, and regarded by Logan 

 and Hunt as au altered bitumen. These pala3ozoic analo- 

 gies would lead us to infer that the larger part of the 

 Laurent ian graphite falls under the second class of de- 

 posits above mentioned, and that, if of vegetable origin, 

 the organic, matter must have been thoroughly disin- 

 tegrated and bituminised before it was changed into 

 graph i to. This would also give a probability that the 

 vegetation implied was aquatic, or at least that it was 

 accumulated under water. 



Dr. Hunt has, however, observed an indication of ter- 

 restrial ve-ctation, or at least of subaerial decay, in the 

 great beds of Laurontian iron-ore. These, if formed in 

 the same manner as more modern deposits of this kind, 

 would imply the reducing and solvent action of sub- 

 stances produced in the decay of plants. In this case 

 such great ore-beds as that of Hull, on the Ottawa, seventy 







x (Jranby, Melbourne, Owl's Head, &c., " Geology of Canada," 1863, 

 p. 599. 



