Return to search

Some aspects of Pleistocene and post-glacial climate change in central Alaska.

One need only see a glacial map of North America to become aware of a curious, if not anomalous fact. For of all the continental vastness four times-buried under the great ice sheets of the Pleistocene epoch, only one land area of any size remained ice free. That was the area of central Alaska and the western Yukon Territory. Here is to be sought the most complete climatic and stratigraphic record of Pleistocene events on the continent, north of the southern border of ice. Within this area, one is fortunate to find a road and transportation network which makes it accessible to the field worker as no other place in North America so far north.

Identiferoai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:QMM.109961
Date January 1955
CreatorsGerard, Robert. D.
ContributorsHare, F. (Supervisor)
PublisherMcGill University
Source SetsLibrary and Archives Canada ETDs Repository / Centre d'archives des thèses électroniques de Bibliothèque et Archives Canada
LanguageEnglish
Detected LanguageEnglish
TypeElectronic Thesis or Dissertation
Formatapplication/pdf
CoverageMaster of Science. (Department of Geography.)
RightsAll items in eScholarship@McGill are protected by copyright with all rights reserved unless otherwise indicated.
Relationalephsysno: NNNNNNNNN, Theses scanned by McGill Library.

Page generated in 0.0023 seconds