A History of New Brunswick Geology
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In our eReader you can find the full English version of the book. Read A History of New Brunswick Geology Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book A History of New Brunswick Geology
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Trappean rocks of Carboniferous and Triassic age. Post Pliocene.
In the general geological map of the southern part of the province, the area colored as Laurentian embraces principally that portion which, in 1860, was separated from the Devonian, under the title of the Portland group. It has, however, since then, been considerably extended ; and west of St. John City, it embraces the greater part of the county of St. John, extending across into Charlotte county, and terminates westward, at Ragg...ed Head, which forms the south-western point of Lepreau Harbor. Though apparently divisible into two unconformable series, it was not deemed advisable to color these se- parately, but the limestones were designated, wherever known to occur, by a distinct tint, and thus the upper member was, tq a certain^ 3 34 NEW BRUNSWICK GEOLOGY.
extent, made conspicuous. The anticlinal structure of the lower mem- ber is well marked, and its probable extension north-easterly has already been given. The limestones in the vicinity of the St.
What to read after A History of New Brunswick Geology?
You can find similar books in the "Read Also" column, or choose other free books by R W Robert Wheelock Ells to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Trappean rocks of Carboniferous and Triassic age. Post Pliocene.
In the general geological map of the southern part of the province, the area colored as Laurentian embraces principally that portion which, in 1860, was separated from the Devonian, under the title of the Portland group. It has, however, since then, been considerably extended ; and west of St. John City, it embraces the greater part of the county of St. John, extending across into Charlotte county, and terminates westward, at Ragg...ed Head, which forms the south-western point of Lepreau Harbor. Though apparently divisible into two unconformable series, it was not deemed advisable to color these se- parately, but the limestones were designated, wherever known to occur, by a distinct tint, and thus the upper member was, tq a certain^ 3 34 NEW BRUNSWICK GEOLOGY.
extent, made conspicuous. The anticlinal structure of the lower mem- ber is well marked, and its probable extension north-easterly has already been given. The limestones in the vicinity of the St.
What to read after A History of New Brunswick Geology?
You can find similar books in the "Read Also" column, or choose other free books by R W Robert Wheelock Ells to read onlineMoreLess
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