Geological Report on Monroe County, Michigan, Band 7R. Smith printing Company, state printers, 1900 - 240 Seiten |
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... PLATES AND EIGHT FIGURES INCLUDING THREE COLORED MAPS PUBLISHED BY AUTHORITY OF THE LAWS OF MICHIGAN UNDER THE DIRECTION OF THE BOARD OF GEOLOGICAL SURVEY LANSING ROBERT SMITH PRINTING CO . , STATE PRINTERS AND BINDERS 1900 Entered ...
... PLATES AND EIGHT FIGURES INCLUDING THREE COLORED MAPS PUBLISHED BY AUTHORITY OF THE LAWS OF MICHIGAN UNDER THE DIRECTION OF THE BOARD OF GEOLOGICAL SURVEY LANSING ROBERT SMITH PRINTING CO . , STATE PRINTERS AND BINDERS 1900 Entered ...
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... the Monroe beds § 4 . Fossils of the Dundee formation 203 203 204 205 206 206 208 209 210 210 211 212 213 214 215 216 217 217 218 220 221 222 226 LIST OF ILLUSTRATIONS . I. Map of Paleozoic Geology PLATES viii MONROE COUNTY .
... the Monroe beds § 4 . Fossils of the Dundee formation 203 203 204 205 206 206 208 209 210 210 211 212 213 214 215 216 217 217 218 220 221 222 226 LIST OF ILLUSTRATIONS . I. Map of Paleozoic Geology PLATES viii MONROE COUNTY .
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William Hittell Sherzer. LIST OF ILLUSTRATIONS . I. Map of Paleozoic Geology PLATES . Page . faces II . South wall of ... Plate I .. FIGURES . 128 140 144 192 ..p . 198 242 1. Mammoth boulder transported by the ice sheet and dropped east ...
William Hittell Sherzer. LIST OF ILLUSTRATIONS . I. Map of Paleozoic Geology PLATES . Page . faces II . South wall of ... Plate I .. FIGURES . 128 140 144 192 ..p . 198 242 1. Mammoth boulder transported by the ice sheet and dropped east ...
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... of the Monroe beds § 4. Fossils of the Dundee formation 203 203 204 205 206 206 208 209 210 210 211 212 213 214 215 216 217 217 218 220 221 222 226 LIST OF ILLUSTRATIONS . PLATES . I. Map of Paleozoic viii MONROE COUNTY .
... of the Monroe beds § 4. Fossils of the Dundee formation 203 203 204 205 206 206 208 209 210 210 211 212 213 214 215 216 217 217 218 220 221 222 226 LIST OF ILLUSTRATIONS . PLATES . I. Map of Paleozoic viii MONROE COUNTY .
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William Hittell Sherzer. LIST OF ILLUSTRATIONS . PLATES . I. Map of Paleozoic Geology II . South wall of the Woolmith ... Plate I .. FIGURES . 198 242 1 . Mammoth boulder transported by the ice sheet and dropped east of the site of Ida ...
William Hittell Sherzer. LIST OF ILLUSTRATIONS . PLATES . I. Map of Paleozoic Geology II . South wall of the Woolmith ... Plate I .. FIGURES . 198 242 1 . Mammoth boulder transported by the ice sheet and dropped east of the site of Ida ...
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Andere Ausgaben - Alle anzeigen
Geological Report on Monroe County, Michigan (Classic Reprint) Will Hittell Sherzer Keine Leseprobe verfügbar - 2018 |
Geological Report on Monroe County, Michigan (Classic Reprint) Will Hittell Sherzer Keine Leseprobe verfügbar - 2018 |
Häufige Begriffe und Wortgruppen
acid alumina anhydrite beach belt beneath blue calcite calcium carbonate carbon dioxide Clair clay color compact Corniferous crystals deposits depth described Detroit dolomite drill Dundee east elevation Erie township feet formation formed fossils fragments Geol Geological Survey gives glacial grains gravel gray Helderberg Huron ice sheet inches iron Lake Erie Lake Shore layers Lenawee Lenawee county lime limestone lower Macon magnesium carbonate Maumee Milan Milan township miles mineral Monroe beds Monroe county moraine northeast northeastward occur Ohio oölite Ottawa Lake outcrop oxide Plate Plum Creek Point aux Peaux portion probably Raisin Raisinville region ridge river road rock Rominger salt sand shale shows silica soil southwest stone Stony Point strata stream striæ strontianite sulphate sulphur Summerfield Summerfield township surface Sylvania Sylvania sandstone thickness tion Toledo township Trenton upper valley Wayne county Whiteford Whiteford township Winchell Woolmith quarry
Beliebte Passagen
Seite 3 - In testimony whereof I have caused these letters to be made patent, and the seal of The United States to be hereunto affixed.
Seite 4 - Miami aforesaid ; and on the north by an east and west line drawn through the southerly extreme of Lake Michigan, running east, after intersecting the due north line aforesaid from the mouth of the Great Miami, until it shall intersect Lake Erie or the territorial line, and thence with the same, through Lake Erie, to the Pennsylvania line...
Seite 4 - ... provided however, and it is further understood and declared, that the boundaries of these three states shall be subject so far to be altered, that, if congress shall hereafter find it expedient, they shall have authority to form one or two states in that part of the said territory which lies north of an east and west line drawn through the southerly bend or extreme of lake Michigan.
Seite 26 - In other words, the shales of our column fill the entire interval between the Hamilton proper and the Catskill group, and in the judgment of some geologists a wider interval even than that named above.
Seite 133 - uplifts" at Little Falls, which rise 147 feet higher than lake Erie, and the "highlands" of the Hudson might also have interposed barriers to an outlet across the state of New York. A single communication only would then exist •with the ocean, viz: through the valley of the Mississippi. That the lakes once discharged their waters in this direction, such additional evidence is furnished by the appearance of the country, that in this our argument, but serves to add confirmation to the general opinion.
Seite 1 - ... the 38th townships to the meridian between the 10th and llth ranges, west of the 4th meridian; thence southerly along the meridian between the 10th and llth ranges to the southern boundary of the said Province of Alberta; thence easterly along the said southern boundary of the Province of Alberta to the south-east corner thereof; thence northerly along the eastern boundary of the said Province of Alberta to the point of commencement. (2) The electoral division of Cardston, bounded as follows:...
Seite 48 - ... 5. Dolomites, magnesites, and magnesian marls, have had their origin in sediments of magnesian carbonate formed by the evaporation of solutions of bicarbonate of magnesia. These solutions have been produced...
Seite 48 - Dolomites, magnesites, and magnesian marls have had their origin in sediments of magnesian carbonate formed by the evaporation of solutions of bicarbonate of magnesia. These solutions have been produced either by the action of bicarbonate of lime upon solutions of sulphate of magnesia, in which case gypsum is a subsidiary product, or by the decomposition of solutions of sulphate or chloride of magnesium by the waters of rivers or springs containing bicarbonate of soda.
Seite 215 - By a fossil is meant any body, or the traces of the existence of any body, whether animal or vegetable, which has been buried in the earth by natural causes.
Seite 4 - ... of the lime and sandrocks, or loose water-worn fragments of still older rocks, swept from the north by the current of a universal ocean and deposited during the general subsidence. Some evidences of the direction of these currents were noticed in my report of last year. Among these are the diluvial furrows and scratches on the surface of the lime rock, the appearance and direction of which correspond with observations made in some of the more eastern states.