. Traces of the Ordovican [sic] system on the Atlantic coast and organic remains of Little River Group, no. IV [microform]. Insects, Fossil; Paleontology; Insectes fossiles; Paléontologie. Section IV., [283 ] Trans. R. S. C. ^lU.— Traces of the Ordovician System on (he Atlantic Const. By 0. v. Matthew, (Hfiwl May 25, 18(W.) In the oarly of tho geology of the of ( ».. he on botweei. tho clirterent grand divisions ol' tho I'lihoo- ZOIC rocks was not very ek'iiily drawn. This aiose partly" tho fact that tiu" ouHior geolo^.ist
. Traces of the Ordovican [sic] system on the Atlantic coast and organic remains of Little River Group, no. IV [microform]. Insects, Fossil; Paleontology; Insectes fossiles; Paléontologie. Section IV., [283 ] Trans. R. S. C. ^lU.— Traces of the Ordovician System on (he Atlantic Const. By 0. v. Matthew, (Hfiwl May 25, 18(W.) In the oarly of tho geology of the of ( ».. he on botweei. tho clirterent grand divisions ol' tho I'lihoo- ZOIC rocks was not very ek'iiily drawn. This aiose partly" tho fact that tiu" ouHior geolo^.ists <irow no ,on between tho Cambrian and Lower SiluriaS (O^dovieianlo between and the Upper ; and partly beeause all the I'aLo- de|,os,t8. exeep, the (", had been greatly disturbed and olded .n almost every part of this region. Owing to these accuracy in the several divisions of the l-ahoo/oR. has also arisen from the scarceness of well proerved iomh, whereby these divisions a,.d their several parts could be distin- guished Iroiu each other. Latterly, and by slow degrees, group after group of the older Paheo- zoic nx-ks have been recognized, and the earlier cla-^siHcation improved J Rep. Prog. Geo). Surv, Can., , Rep. G, p. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Matthew, G. F. (George Frederick), 1837-1923. Ottawa : J. Durie
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Keywords: ., bookcentury1800, bookdecad, booksubjectpaleontology, bookyear1895
