The ice age in North America and its bearing upon the antiquity of man5th edwith many new maps and illus., enland rewritten to incorporate the facts that bring it up to date, with chapters on Lake Agassiz and the Probable cause of glaciation . 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 Eve
The ice age in North America and its bearing upon the antiquity of man5th edwith many new maps and illus., enland rewritten to incorporate the facts that bring it up to date, with chapters on Lake Agassiz and the Probable cause of glaciation . 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, 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 all essential characteristics they are identical in may be their relations in time remains to be determined.
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