The Journal of Geology, Volume 15

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Thomas Chrowder Chamberlin
University of Chicago Press, 1907
Vols. for 1893-1923 includes section: "Reviews."

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Page 673 - A New Batrachian and a New Reptile from the Trias of Arizona,
Page 837 - Remittances should be made payable to The University of Chicago Press, and should be in Chicago or New York exchange, postal or express money order. If local check is used, 10 cents must be added for collection. The following agents have been appointed and are authorized to quote the prices indicated: For the British Empire: The Cambridge University Press, Fetter Lane, London, EG, England.
Page 725 - Failure of wells along the Lower Huron river, Michigan, in 1904, by Myron L. Fuller, 29 pp.; 1. Water supplies of the Lower Huron river district, 2. Decline of water supplies of the wells, 3. Necessity of laws for regulating deep or artesian wells; (b) Geological reconnaissance along the north shore of lakes Huron and Michigan, by IC Russell.
Page 409 - Range,' is separated from the 1 Published by permission of the Director of the US Geological Survey. The accompanying map has been redrawn and adapted from the field map prepared in 1906 by my associate in the field, Mr. AG Maddren. Certain additions are based on photographs and surveys by Mr. AJ Brabazon, of the Canadian Boundary Survey.
Page 837 - Reprints of leading articles will be printed as ordered, the actual cost (with cover, if desired) to be paid for by the author. Reprints must be paid for when ordered. The table below shows the approximate cost of reprints consisting of plain text or text with line engravings. The actual cost may vary from the figures given, and will depend upon the amount of work in re-making the pages into forms, press work, paper, binding, etc.
Page 726 - WARD, LESTER F. Status of the Mesozoic floras of the United States. Second paper by Lester F. Ward, with the collaboration of William M. Fontaine, Arthur Bibbins, and GR Wieland.
Page 509 - A Monograph of the Carboniferous and Permo-Carboniferous Invertebrata of New South Wales.
Page 792 - While the ice responded to topography, and in a large measure was controlled by the physical features of the range, yet at the same time it was modifying the forms encountered, changing the shape of the great canyons, and building new forms. Before the first Pleistocene snows fell on the Uinta Mountains, the heads of the great canyons may be fairly assumed to have been narrow V-shaped notches, reaching in most cases nearly to the crest-line of the range.

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