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- W2101538350 abstract "Research Article| May 01, 1987 Glaciation and the evolution of the Canadian high arctic landscape John England John England 1Department of Geography, University of Alberta, Edmonton, Alberta T6G 2H4, Canada Search for other works by this author on: GSW Google Scholar Author and Article Information John England 1Department of Geography, University of Alberta, Edmonton, Alberta T6G 2H4, Canada Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1987) 15 (5): 419–424. https://doi.org/10.1130/0091-7613(1987)15<419:GATEOT>2.0.CO;2 Article history First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation John England; Glaciation and the evolution of the Canadian high arctic landscape. Geology 1987;; 15 (5): 419–424. doi: https://doi.org/10.1130/0091-7613(1987)15<419:GATEOT>2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract The Canadian arctic islands represent a Tertiary fluvial landscape developed on a contiguous landmass subsequently fractured by block faulting. Nonetheless, some theoretical models invoke pervasive high-latitude ice sheets and continue to misattribute the faulted landscape to glacially scoured river valleys. Quaternary fieldwork on northern Ellesmere Island suggests that these models are inappropriate for high-latitude ice sheets and should be abandoned. If there was ever a regional ice sheet over arctic Canada, it likely occurred on a prefaulted, contiguous landmass that had a more temperate climate than at present, possibly during the late Tertiary. After block faulting, the marine channels permanently prevented the ice from inundating the landscape it once crossed. Tectonics, and not climate, have led to a fundamental change in glacial style. This block faulting also may have played a role in terminating the late Tertiary boreal forest (to ∼80°N) by establishing cold marine channels that diminished the continentality of the once-contiguous landmass. For a thorough understanding of the Canadian arctic landscape, future research should determine the continuity between the Tertiary and Quaternary paleoenvironments. The unknown ages of the fiords and interisland channels are of primary importance. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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- W2101538350 title "Glaciation and the evolution of the Canadian high arctic landscape" @default.
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