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File:Glacial formations and drainage features of the Erie and Ohio basins (1902) (14597307459).jpg

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Identifier: glacialformation00leve (find matches)
Title: Glacial formations and drainage features of the Erie and Ohio basins
Year: 1902 (1900s)
Authors: Leverett, Frank, 1859-1943
Subjects: Glacial epoch Geology
Publisher: Washington, : Govt. Print. Off.
Contributing Library: University of Connecticut Libraries
Digitizing Sponsor: Boston Library Consortium Member Libraries

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ognized drift sheet and the final recession of the icesheet into the region north of the Great Lakes. The main divisions appearto be much longer than the secondary ones. .The latter are not thought tobe marked by intervals sufficiently prolonged to merit the application ofthe term epoch. It is probable, however, as shown further on, that someoscillations of the ice front occurred, so that the moraines on which thesesubdivisions are based do not mark simply halts in the recession of the ice. OUTIiIXE OF DRIFT SHEETS AND INTERVALS. 1. Oldest recognized drift sheet, the sub-Aftonian of Chamberhn, and perhaps the Albertan of Dawson. 2. First interval of deglaciation, Aftonian of Chamberlin. 3. Kansan drift sheet of the Iowa geologists. iThe Illinois Glacial Lobe, Mon. U. S. Geol. Survey, Vol. XXXVIII. ■See Geikies Great Ice Age, third edition, 1894, pp. 754-774. See also Jour. Geol., Vol. Ill, pp.270-277, and Vol. IV, pp. 872-876. U S GEOLOGICAL SURVEY MONOGRAPH XLI PL MICHIGAN KFCTLCKl
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  • bookid:glacialformation00leve
  • bookyear:1902
  • bookdecade:1900
  • bookcentury:1900
  • bookauthor:Leverett__Frank__1859_1943
  • booksubject:Glacial_epoch
  • booksubject:Geology
  • bookpublisher:Washington____Govt__Print__Off_
  • bookcontributor:University_of_Connecticut_Libraries
  • booksponsor:Boston_Library_Consortium_Member_Libraries
  • bookleafnumber:57
  • bookcollection:uconn_libraries
  • bookcollection:blc
  • bookcollection:americana
  • BHL Collection
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30 July 2014


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