. Acadian geology [microform] : the geological structure, organic remains and mineral resources of Nova Scotia, New Brunswick and Prince Edward Island. Geology; Paleontology; Geology; Geology; Geologie; Paléontologie; Géologie; Géologie. t seem to be a I, and directly the nature and Lindancc of pale f intcrstratified id indicates an 5 the line of the is little known, â obably forming along the New lal Map.) vn to occupy an ver, along both would seem to entire peninsula nay be traced to [rating at Dickie stance below the side of the latter, the Belleisle and variable in corn- exhibiting some
. Acadian geology [microform] : the geological structure, organic remains and mineral resources of Nova Scotia, New Brunswick and Prince Edward Island. Geology; Paleontology; Geology; Geology; Geologie; Paléontologie; Géologie; Géologie. t seem to be a I, and directly the nature and Lindancc of pale f intcrstratified id indicates an 5 the line of the is little known, â obably forming along the New lal Map.) vn to occupy an ver, along both would seem to entire peninsula nay be traced to [rating at Dickie stance below the side of the latter, the Belleisle and variable in corn- exhibiting some the deposits of bed in detail, as nd Kars. The age and strati- 'essor Bailey to n the following Hunt does not lada. They are principal series no hesitation in which I believe he rocks of the jrn Nova Scotia, 'his is the ago to NEW BRUNSWICK, 877 which T would therefore be inclined to refer your rc/Ks, though I would not afBrm that they may not include Lower Devonian, which in Nova Scotia are altered with the Upper Silurian. " I regard your specimens as altered sediments, though some of the felspathic and homblendic ones may be true Plutonic ; (2.) Mr Matthew has found, in loose fragments, near St John, pro- bably derived from these rocks, the following fossils:âChonetes, Pterinea or Avicula, Clidophorus, Oi'this, Rhynchonella (?), Leptodo' mus (?), etc.; and still more recently specimens have been obtained from undoubted members of the Kingston group, in which the follow- ing characteristic Upper Silurian assemblage of genera occurs, though in a state too imperfect for specific determination. The genera are Dalmania, Phacops, Orthoceras (2 species), Murchi- sonia (2 species), Loxonema, Holopea (?), Lucina (?) or Anatina (?), Avicula (?), Leptodomus (?), Sph'ifer, Chonetes (?), Atrypa, Rhyn- chonella (?), Retzia (?), Strophomena, Orthi's, Dischia, Favosites, Zaphrentis (2 species), Syringopora (?), and other corals. From Frye's Island also, in the south-
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Keywords: ., boo, bookcentury1800, booksubjectgeology, booksubjectpaleontology
