A History of the State of Ohio: Natural and CivilSterotyped by Glezen & Shepard, 1838 - 403 Seiten |
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Seite 10
... whole valley of the Mississippi , is what Geologists de- nominate " a secondary formation . " Those who have written on Geology , may be divided into two classes , Huttonians and Wernerians , from Hutton and Werner , the founders of the ...
... whole valley of the Mississippi , is what Geologists de- nominate " a secondary formation . " Those who have written on Geology , may be divided into two classes , Huttonians and Wernerians , from Hutton and Werner , the founders of the ...
Seite 11
... whole valley , is covered , to a vast depth , with the ruins of a former world . This is the greatest valley , and the largest tract of secondary formation , in the whole world . This vast field has been but recently visited by ...
... whole valley , is covered , to a vast depth , with the ruins of a former world . This is the greatest valley , and the largest tract of secondary formation , in the whole world . This vast field has been but recently visited by ...
Seite 12
... whole belt of land , near- est the lake , is composed of sand and water worn pebbles , all along its southern shore . The strip of land , which we have described , is elevated about seventy feet above the present surface of the Erie ...
... whole belt of land , near- est the lake , is composed of sand and water worn pebbles , all along its southern shore . The strip of land , which we have described , is elevated about seventy feet above the present surface of the Erie ...
Seite 13
... whole , it may be fairly estimated , at eight hundred feet . Its surface is infinitely varied , in its hilly region ; sometimes it rises into abrupt precipices , in the sandstone regions , and then again , falling off , into long plates ...
... whole , it may be fairly estimated , at eight hundred feet . Its surface is infinitely varied , in its hilly region ; sometimes it rises into abrupt precipices , in the sandstone regions , and then again , falling off , into long plates ...
Seite 14
... whole series . Hence , it is inferred , that these hills and pillars , once con- stituted a continuous mass , traversed by perpendicular fissures , and that the elements have operated the changes in them which we now see . Along the ...
... whole series . Hence , it is inferred , that these hills and pillars , once con- stituted a continuous mass , traversed by perpendicular fissures , and that the elements have operated the changes in them which we now see . Along the ...
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