New Evidence of a Post-Laurentide Local Cirque Glacier on Mount Washington, New Hampshire

As global temperatures warmed and the last North American continental ice sheet receded there were several climate reversals during which time mean temperatures in New England were significantly reduced. Decreased temperatures in combination with increased precipitation may have supported the format...

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Bibliographic Details
Main Authors: Dulin, Ian T., Fowler, Brian K., Cook, Timothy L.
Format: Text
Language:unknown
Published: SCARAB 2012
Subjects:
cirque
glacier
Mount Washington
climate
Geology
Ela
Ice Sheet
Online Access:https://scarab.bates.edu/honorstheses/20
https://scarab.bates.edu/cgi/viewcontent.cgi?article=1052&context=honorstheses

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