Journal And Proceedings of the Royal Society of New South Wales 17
Journal And Proceedings of the Royal Society of New South Wales 17
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In our eReader you can find the full English version of the book. Read Journal And Proceedings of the Royal Society of New South Wales 17 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 Journal And Proceedings of the Royal Society of New South Wales 17
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Darwin's theory of coral islands.
In one instance I succeeded in finding, in 9Uu beneath the cmst of coral- rock, the crystalline eruptive rock of the original island before it underwent subsidence and became clothed with coraL The island of UjB;i presents yet another variety of geological structure : a low-lyinff island, it is composed of bedded f oraminif erous limestone — once incrusted with coral-rock, which is now to a great extent removed by denudation : flints occur in the surface soil— ...though I have not yet found them in situ. I intend however to continue my observations on this island.
Professor Liversidge remarked that some years ago Mr. Brown, the Wesleyan missionary, brought from New Britain a soft wliite limestone which was quite undistinguishable from chalk, not only physically but chemically, and pointed out that this discovery of flints afforded another very strong proof of the probable presence of true chalk of Cretaceous age in the South Sea Islands.* Samples of Water from tJie Islands of Simbo and Santa Anna, collected by Dr.
What to read after Journal And Proceedings of the Royal Society of New South Wales 17?
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To quickly assess the difficulty of the text, read a short excerpt:
Darwin's theory of coral islands.
In one instance I succeeded in finding, in 9Uu beneath the cmst of coral- rock, the crystalline eruptive rock of the original island before it underwent subsidence and became clothed with coraL The island of UjB;i presents yet another variety of geological structure : a low-lyinff island, it is composed of bedded f oraminif erous limestone — once incrusted with coral-rock, which is now to a great extent removed by denudation : flints occur in the surface soil— ...though I have not yet found them in situ. I intend however to continue my observations on this island.
Professor Liversidge remarked that some years ago Mr. Brown, the Wesleyan missionary, brought from New Britain a soft wliite limestone which was quite undistinguishable from chalk, not only physically but chemically, and pointed out that this discovery of flints afforded another very strong proof of the probable presence of true chalk of Cretaceous age in the South Sea Islands.* Samples of Water from tJie Islands of Simbo and Santa Anna, collected by Dr.
What to read after Journal And Proceedings of the Royal Society of New South Wales 17?
You can find similar books in the "Read Also" column, or choose other free books by Royal Society of New South Wales to read onlineMoreLess
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