2012, ISBN: 1130470814

[EAN: 9781130470819], Neubuch, [PU: Rarebooksclub.com, United States], Language: English Brand New Book ***** Print on Demand *****. This historic book may have numerous typos and missing… mais…

[EAN: 9781130470819], Neubuch, [PU: Rarebooksclub.com, United States], Language: English Brand New Book ***** Print on Demand *****. This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1918 Excerpt: .had shifted somewhat and had readvanced to the moraines grouped by Chamberlin with the Kettle moraine. In Illinois these earlier moraines spread out widely, indicating a considerably greater extension of the early Wisconsin ice than at the later readvance. In northern Illinois, in Kane and McHenry counties, the moraines are crowded together into a single continuous belt, showing that the extension of the earlier ice was restricted, and that at the succeeding substages the ice crowded forward nearly to the same limit. The Valparaiso morainic system of the later Wisconsin glacier orowds in with the others, so as to form the eastern part of the belt. Extending northward into Wisconsin in a reentrant angle near Fox River the correlatives of the Valparaiso recurve sharply and pass about the head of Lake Geneva to the inter-lobate angle in the vicinity of Richmond, in western Walworth County, where they join the terminal moraine of the Green Bay Glacier. As shown by Chamberlin in 1876 2 and later described more fully by the present writer,3 these moraines circumscribe a small lobe of the Lake Michigan Glacier which extended from the angle of convergence of the fronts of the Lake Michigan and Green Bay glaciers in such a way as to override the northward extension of the earlier Wisconsin moraines in the vicinity of the State line. Thus the outer terminal moraines of the Green Bay Glacier and of the Delavan lobe of the Lake Michigan 1 Leverett, Frank, The Illinois glacial lobe: U. S. Geol. Survey Mon. 38, pp. 20-21,1899. 2 Geology of Wisconsin, vol. 2, pl. 7,1877. s Alden, W. C, The Delavan lobe ol the Lake Michigan Glacier of the Wisconsin stage of glaciation: U.S. Geol. Survey Prof. Paper 34,1904. Glacier are believed to be the correlatives of the Valparaiso mora.<

2012, ISBN: 1130470814

[EAN: 9781130470819], Neubuch, [PU: Rarebooksclub.com, United States], Language: English Brand New Book ***** Print on Demand *****.This historic book may have numerous typos and missing … mais…

[EAN: 9781130470819], Neubuch, [PU: Rarebooksclub.com, United States], Language: English Brand New Book ***** Print on Demand *****.This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1918 Excerpt: .had shifted somewhat and had readvanced to the moraines grouped by Chamberlin with the Kettle moraine. In Illinois these earlier moraines spread out widely, indicating a considerably greater extension of the early Wisconsin ice than at the later readvance. In northern Illinois, in Kane and McHenry counties, the moraines are crowded together into a single continuous belt, showing that the extension of the earlier ice was restricted, and that at the succeeding substages the ice crowded forward nearly to the same limit. The Valparaiso morainic system of the later Wisconsin glacier orowds in with the others, so as to form the eastern part of the belt. Extending northward into Wisconsin in a reentrant angle near Fox River the correlatives of the Valparaiso recurve sharply and pass about the head of Lake Geneva to the inter-lobate angle in the vicinity of Richmond, in western Walworth County, where they join the terminal moraine of the Green Bay Glacier. As shown by Chamberlin in 1876 2 and later described more fully by the present writer,3 these moraines circumscribe a small lobe of the Lake Michigan Glacier which extended from the angle of convergence of the fronts of the Lake Michigan and Green Bay glaciers in such a way as to override the northward extension of the earlier Wisconsin moraines in the vicinity of the State line. Thus the outer terminal moraines of the Green Bay Glacier and of the Delavan lobe of the Lake Michigan 1 Leverett, Frank, The Illinois glacial lobe: U. S. Geol. Survey Mon. 38, pp. 20-21,1899. 2 Geology of Wisconsin, vol. 2, pl. 7,1877. s Alden, W. C, The Delavan lobe ol the Lake Michigan Glacier of the Wisconsin stage of glaciation: U.S. Geol. Survey Prof. Paper 34,1904. Glacier are believed to be the correlatives of the Valparaiso mora.<

ISBN: 1130470814

[EAN: 9781130470819], Neubuch, GEOLOGICAL SURVEY,SUBJECTS, This item is printed on demand. Paperback. This historic book may have numerous typos and missing text. Purchasers can download … mais…

[EAN: 9781130470819], Neubuch, GEOLOGICAL SURVEY,SUBJECTS, This item is printed on demand. Paperback. This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1918 Excerpt: . . . had shifted somewhat and had readvanced to the moraines grouped by Chamberlin with the Kettle moraine. In Illinois these earlier moraines spread out widely, indicating a considerably greater extension of the early Wisconsin ice than at the later readvance. In northern Illinois, in Kane and McHenry counties, the moraines are crowded together into a single continuous belt, showing that the extension of the earlier ice was restricted, and that at the succeeding substages the ice crowded forward nearly to the same limit. The Valparaiso morainic system of the later Wisconsin glacier orowds in with the others, so as to form the eastern part of the belt. Extending northward into Wisconsin in a reentrant angle near Fox River the correlatives of the Valparaiso recurve sharply and pass about the head of Lake Geneva to the inter-lobate angle in the vicinity of Richmond, in western Walworth County, where they join the terminal moraine of the Green Bay Glacier. As shown by Chamberlin in 1876 2 and later described more fully by the present writer, 3 these moraines circumscribe a small lobe of the Lake Michigan Glacier which extended from the angle of convergence of the fronts of the Lake Michigan and Green Bay glaciers in such a way as to override the northward extension of the earlier Wisconsin moraines in the vicinity of the State line. Thus the outer terminal moraines of the Green Bay Glacier and of the Delavan lobe of the Lake Michigan 1 Leverett, Frank, The Illinois glacial lobe: U. S. Geol. Survey Mon. 38, pp. 20-21, 1899. 2 Geology of Wisconsin, vol. 2, pl. 7, 1877. s Alden, W. C, The Delavan lobe ol the Lake Michigan Glacier of the Wisconsin stage of glaciation: U. S. Geol. Survey Prof. Paper 34, 1904. Glacier are believed to be the correlatives of the Valparaiso mora. . . This item ships from La Vergne,TN.<

2012, ISBN: 1130470814

[EAN: 9781130470819], Neubuch, [PU: Rarebooksclub.com, United States], Brand New Book ***** Print on Demand *****. This historic book may have numerous typos and missing text. Purchasers … mais…

[EAN: 9781130470819], Neubuch, [PU: Rarebooksclub.com, United States], Brand New Book ***** Print on Demand *****. This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1918 Excerpt: .had shifted somewhat and had readvanced to the moraines grouped by Chamberlin with the Kettle moraine. In Illinois these earlier moraines spread out widely, indicating a considerably greater extension of the early Wisconsin ice than at the later readvance. In northern Illinois, in Kane and McHenry counties, the moraines are crowded together into a single continuous belt, showing that the extension of the earlier ice was restricted, and that at the succeeding substages the ice crowded forward nearly to the same limit. The Valparaiso morainic system of the later Wisconsin glacier orowds in with the others, so as to form the eastern part of the belt. Extending northward into Wisconsin in a reentrant angle near Fox River the correlatives of the Valparaiso recurve sharply and pass about the head of Lake Geneva to the inter-lobate angle in the vicinity of Richmond, in western Walworth County, where they join the terminal moraine of the Green Bay Glacier. As shown by Chamberlin in 1876 2 and later described more fully by the present writer,3 these moraines circumscribe a small lobe of the Lake Michigan Glacier which extended from the angle of convergence of the fronts of the Lake Michigan and Green Bay glaciers in such a way as to override the northward extension of the earlier Wisconsin moraines in the vicinity of the State line. Thus the outer terminal moraines of the Green Bay Glacier and of the Delavan lobe of the Lake Michigan 1 Leverett, Frank, The Illinois glacial lobe: U. S. Geol. Survey Mon. 38, pp. 20-21,1899. 2 Geology of Wisconsin, vol. 2, pl. 7,1877. s Alden, W. C, The Delavan lobe ol the Lake Michigan Glacier of the Wisconsin stage of glaciation: U.S. Geol. Survey Prof. Paper 34,1904. Glacier are believed to be the correlatives of the Valparaiso mora.<

2012, ISBN: 1130470814

[EAN: 9781130470819], Neubuch, [PU: Rarebooksclub.com, United States], Brand New Book ***** Print on Demand *****.This historic book may have numerous typos and missing text. Purchasers c… mais…

[EAN: 9781130470819], Neubuch, [PU: Rarebooksclub.com, United States], Brand New Book ***** Print on Demand *****.This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1918 Excerpt: .had shifted somewhat and had readvanced to the moraines grouped by Chamberlin with the Kettle moraine. In Illinois these earlier moraines spread out widely, indicating a considerably greater extension of the early Wisconsin ice than at the later readvance. In northern Illinois, in Kane and McHenry counties, the moraines are crowded together into a single continuous belt, showing that the extension of the earlier ice was restricted, and that at the succeeding substages the ice crowded forward nearly to the same limit. The Valparaiso morainic system of the later Wisconsin glacier orowds in with the others, so as to form the eastern part of the belt. Extending northward into Wisconsin in a reentrant angle near Fox River the correlatives of the Valparaiso recurve sharply and pass about the head of Lake Geneva to the inter-lobate angle in the vicinity of Richmond, in western Walworth County, where they join the terminal moraine of the Green Bay Glacier. As shown by Chamberlin in 1876 2 and later described more fully by the present writer,3 these moraines circumscribe a small lobe of the Lake Michigan Glacier which extended from the angle of convergence of the fronts of the Lake Michigan and Green Bay glaciers in such a way as to override the northward extension of the earlier Wisconsin moraines in the vicinity of the State line. Thus the outer terminal moraines of the Green Bay Glacier and of the Delavan lobe of the Lake Michigan 1 Leverett, Frank, The Illinois glacial lobe: U. S. Geol. Survey Mon. 38, pp. 20-21,1899. 2 Geology of Wisconsin, vol. 2, pl. 7,1877. s Alden, W. C, The Delavan lobe ol the Lake Michigan Glacier of the Wisconsin stage of glaciation: U.S. Geol. Survey Prof. Paper 34,1904. Glacier are believed to be the correlatives of the Valparaiso mora.<