Education Department Bulletin, Issues 434-436University of the State of New York, 1908 - Education |
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... tion .... Topographic features .. General geology ... Stratigraphic relations of the Clinton formation ... General structure .. 57 8 9 II ∞OE FO II The ores .. Mineralogy and structural fea- tures ... Chemical character .. Origin of ...
... tion .... Topographic features .. General geology ... Stratigraphic relations of the Clinton formation ... General structure .. 57 8 9 II ∞OE FO II The ores .. Mineralogy and structural fea- tures ... Chemical character .. Origin of ...
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... tion , specially to the west , where the strata continue for a long distance with scarcely perceptible changes . The outcrop nar- rows more quickly toward the east mainly on account of the increasing inclination of the beds in that ...
... tion , specially to the west , where the strata continue for a long distance with scarcely perceptible changes . The outcrop nar- rows more quickly toward the east mainly on account of the increasing inclination of the beds in that ...
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... tion , whereby each member has had a wider area of deposition than the one immediately preceding . The general relations will be readily understood from the accompanying diagram . It will be ob- served that there is one exception to the ...
... tion , whereby each member has had a wider area of deposition than the one immediately preceding . The general relations will be readily understood from the accompanying diagram . It will be ob- served that there is one exception to the ...
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... tion of salt and gypsum . These conditions may have been initiated even as early as Medina time . Salt springs are found not infre- quently along the outcrop of the Medina sandstones and in such a state of concentration that they were ...
... tion of salt and gypsum . These conditions may have been initiated even as early as Medina time . Salt springs are found not infre- quently along the outcrop of the Medina sandstones and in such a state of concentration that they were ...
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... tion may have been furnished by the Paleozoic sediments fringing the crystalline areas and previously upraised above sea level . But as these sediments are for the most part low in iron , it is to the Precambric gneisses and schists ...
... tion may have been furnished by the Paleozoic sediments fringing the crystalline areas and previously upraised above sea level . But as these sediments are for the most part low in iron , it is to the Precambric gneisses and schists ...
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12 July 13 June 27 June 9 Apr 9 Mar Adds Agric Amds annual appointed by Gov assmt Atty Auditor bank bond certificate clerk Clinton common carrier Comn Const corp corporations County Court Declaring unconst deposits Dept election eminent domain employees erect examination f g h fees feet fossil fund hematite inches inspection insurance company investigate iron Joint legis July June Wis justice of peace land Library license lien limestone liquor Mass miles mining Msdr N. Y. Amdg officers Oneida Oneida county oolitic outcrop penalty person Prohibiting Railroad Comrs regulations report to Gov Revisal 05 salary sandstone Senate shale Siluric subdiv Submitting amdt Supreme Court Supt taxation Tenn tion town trustees veterans Vote Nov Wash
Popular passages
Page 261 - An act for preventing the manufacture, sale, or transportation of adulterated or misbranded, or poisonous, or deleterious foods, drugs, medicines, and liquors, and for regulating traffic therein, and for other purposes...
Page 592 - DANIEL BEACH Ph.D. LL.D. - Watkins 1914 PLINY T. SEXTON LL.B. LL.D. - ... Palmyra 1912 T. GUILFORD SMITH MACE LL.D. - - - Buffalo 1918 WILLIAM NOTTINGHAM MA Ph.D. LL.D. - - Syracuse 1910 CHARLES A. GARDINER Ph.DLHD LL.DDCL New York 1915 ALBERT VANDER VEER MDMA Ph.D.
Page 262 - March 11, 1908, and to repeal section 15-a of an act entitled an act to prevent the manufacture or sale of adulterated, misbranded, poisonous or deleterious stock and cattle feeds, and to repeal section 15 and sub-sections a, b, c.
Page 4 - Bibliotheca Hispana Vetus, sive hispani scriptores qui ab Octaviani Augusti aevo ad annum Christi MD.