File:The ice age in North America and its bearing upon the antiquity of man. 5th ed. with many new maps and illus., enl. and rewritten to incorporate the facts that bring it up to date, with chapters on (14595826239).jpg

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Identifier: iceageinnorthame00wriguoft (find matches)
Title: The ice age in North America and its bearing upon the antiquity of man. 5th ed. with many new maps and illus., enl. and rewritten to incorporate the facts that bring it up to date, with chapters on Lake Agassiz and the Probable cause of glaciation
Year: 1911 (1910s)
Authors: Wright, G. Frederick (George Frederick), 1838-1921 Upham, Warren, 1850-1934
Subjects: Glacial epoch Glaciers
Publisher: Oberlin, Ohio Bibliotheca Sacra Co
Contributing Library: Gerstein - University of Toronto
Digitizing Sponsor: MSN

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ding See, near the boundary of Poland. Among the places where this moraine can be best seenare— 1. In Province Holstein, the region about (especiallynorth of) Eutin; 2. Province Mecklenburg, north of Crivitz,and between Biitow and Kropelin ; 3. Province Brandenburg,south of Reckatel, between Strassen and Biirenbusch, southof Fiirstenberg and north of Everswalde, and between Pyritzand Solden; 4. Province Posen, east of Locknitz, and atnumerous points to the south, and especially about Falkenburg,and between Lompelburg and Barwalde. This is one of thebest localities. 5. Province West Preussen, east of Biitow;6. Province Ost Preussen, between Horn and Widikin. Comparing these with the moraines of America, ProfessorSalisbury remarks: In its composition from several members, in its variety ofdevelopment, in its topographic relations, in its topography, in * Professor R. D. Salisbury on Terminal Moraines in Northern Germany,in Anipric-an Journal of Science, vol. cxxxv, 1888, pp. 405, 406.
Text Appearing After Image:
X M 458 THE ICE AGE IN NORTH AMERICA. its constitution, in its associated deposits, and in its wide sep-aration from the outermost drift limit, this morainic belt cor-responds to the extensive morainic belt of America, whichextends from Dakota to the Atlantic Ocean. That the oneformation corresponds to the other does not admit of doubt.In all essential characteristics they are identical in character.What may be their relations in time remains to be determined.

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