Geologic Framework and Glaciation of the Eastern Area

Late Pleistocene landscapes in glaciated eastern North America include changing ice margins, fluctuating lake and sea levels, and deglaciated physical settings that were inhabited by a variety of extinct (Rancholabrean) fauna. The glaciated East of North America consists of the mid-continent from Hu...

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Bibliographic Details
Main Author: Hill, Christopher L.
Format: Text
Language:unknown
Published: ScholarWorks 2006
Subjects:
Online Access:https://scholarworks.boisestate.edu/anthro_facpubs/72
https://scholarworks.boisestate.edu/context/anthro_facpubs/article/1071/viewcontent/HillEasternLWEdit.pdf
Description
Summary:Late Pleistocene landscapes in glaciated eastern North America include changing ice margins, fluctuating lake and sea levels, and deglaciated physical settings that were inhabited by a variety of extinct (Rancholabrean) fauna. The glaciated East of North America consists of the mid-continent from Hudson Bay to south of the Great Lakes and extends eastward to the Atlantic coast. Glaciers were present along the Atlantic coast from southern New York north to Labrador.