Geological Report on Monroe County, Michigan, Band 7R. Smith printing Company, state printers, 1900 - 240 Seiten |
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Seite 5
... to recent sub- mergence by the Lake . Photographed , August , 1890 6 . 146 \ 148 View of extensive Cranberry marsh when flooded in the spring . Sec . 24 , Summerfield township 157 B Page . § 5. Cement materials § 6. Road metal Page.
... to recent sub- mergence by the Lake . Photographed , August , 1890 6 . 146 \ 148 View of extensive Cranberry marsh when flooded in the spring . Sec . 24 , Summerfield township 157 B Page . § 5. Cement materials § 6. Road metal Page.
Seite 7
... - mergence by the Lake . Photographed , August , 1890 " 6. View of extensive Cranberry marsh when flooded in the spring . Sec . 24 , Summerfield township 148 157 B Page . 7. Gushing well struck upon Otter Creek , Page.
... - mergence by the Lake . Photographed , August , 1890 " 6. View of extensive Cranberry marsh when flooded in the spring . Sec . 24 , Summerfield township 148 157 B Page . 7. Gushing well struck upon Otter Creek , Page.
Seite 1
... townships between 41 ° 44 ′ and 42 ° 6 ′ , north latitude ; and between 83 ° 11 ′ and 83 ° 46 ' , west longitude ... township . Having the same general direction as all of the preceding and the common purpose of centering in Detroit ...
... townships between 41 ° 44 ′ and 42 ° 6 ′ , north latitude ; and between 83 ° 11 ′ and 83 ° 46 ' , west longitude ... township . Having the same general direction as all of the preceding and the common purpose of centering in Detroit ...
Seite 2
... township . It is reported to be the intention of the promoters of this road to construct a line from Milan , through Dundee , to Toledo . Still an- other road , with branches from Ann Arbor and Detroit , is expected to enter the county ...
... township . It is reported to be the intention of the promoters of this road to construct a line from Milan , through Dundee , to Toledo . Still an- other road , with branches from Ann Arbor and Detroit , is expected to enter the county ...
Seite 3
... townships of the county , their postoffices and some miscellaneous information relating to them , gathered from latest available sources . It shows the popula- tion in 1894 to have been 33,181 . The city of Monroe is the county . seat ...
... townships of the county , their postoffices and some miscellaneous information relating to them , gathered from latest available sources . It shows the popula- tion in 1894 to have been 33,181 . The city of Monroe is the county . seat ...
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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 anhydrite beach belt beneath bituminous blue bluish boulders calcite calcium carbonate Clair clay color compact Corniferous crystals deposits depth described Detroit dolomite drab drift drill Dundee east elevation formation formed fossils fragments Geol Geological Survey gravel gray Helderberg Huron ice sheet inches iron Lake Erie Lake Shore layers Lenawee Lenawee county lime limestone lower Macon magnesium carbonate Maumee Michigan Milan Milan township miles mineral Monroe beds Monroe county moraine northeast northeastward occur Ohio one-half oölite Ottawa Lake outcrop oxide Plate Plum Creek Point aux Peaux portion probably quarry quartz Raisin Raisinville region ridge river River Raisin road rock Rominger salt sandstone shale shows silica soil southeastern southwest stone Stony Point strata stream striæ strontianite sulphate sulphur Summerfield Summerfield township surface Sylvania Sylvania sandstone tion Toledo township Traverse Trenton upper 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 135 - 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 217 - 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.