The Cordilleran Ice Sheet developed over British Columbia and surrounding areas repeatedly during the Pleistocene and most recently during Marine Oxygen Isotope Stage 2 (ca. 25-10 ka). Landforms and deposits of the last glaciation are dominant surface materials; older glacial sediments locally occur below the last-glacial sediments. The ice sheet deformed the lithosphere on which in rested; the deformation is captured in raised and deformed marine and lake shorelines.
%0 Book Section
%1 clague2011chapter
%A Clague, John J.
%A Ward, Brent
%B Quaternary Glaciations - Extent and Chronology
%D 2011
%E Ehlers, Jürgen
%E Gibbard, Philip L.
%E Hughes, Philip D.
%I Elsevier
%K LGM Pleistocene glaciation
%P 563 - 573
%R https://doi.org/10.1016/B978-0-444-53447-7.00044-1
%T Pleistocene Glaciation of British Columbia
%U http://www.sciencedirect.com/science/article/pii/B9780444534477000441
%V 15
%X The Cordilleran Ice Sheet developed over British Columbia and surrounding areas repeatedly during the Pleistocene and most recently during Marine Oxygen Isotope Stage 2 (ca. 25-10 ka). Landforms and deposits of the last glaciation are dominant surface materials; older glacial sediments locally occur below the last-glacial sediments. The ice sheet deformed the lithosphere on which in rested; the deformation is captured in raised and deformed marine and lake shorelines.
@incollection{clague2011chapter,
abstract = {The Cordilleran Ice Sheet developed over British Columbia and surrounding areas repeatedly during the Pleistocene and most recently during Marine Oxygen Isotope Stage 2 (ca. 25-10 ka). Landforms and deposits of the last glaciation are dominant surface materials; older glacial sediments locally occur below the last-glacial sediments. The ice sheet deformed the lithosphere on which in rested; the deformation is captured in raised and deformed marine and lake shorelines.},
added-at = {2019-01-20T05:15:04.000+0100},
author = {Clague, John J. and Ward, Brent},
biburl = {https://www.bibsonomy.org/bibtex/2e30133d893c4ed9a1ff2a5eb21e96cd1/peter.ralph},
booktitle = {Quaternary Glaciations - Extent and Chronology},
doi = {https://doi.org/10.1016/B978-0-444-53447-7.00044-1},
editor = {Ehlers, Jürgen and Gibbard, Philip L. and Hughes, Philip D.},
interhash = {822632f684f976856c1ddaee8dc990a0},
intrahash = {e30133d893c4ed9a1ff2a5eb21e96cd1},
issn = {1571-0866},
keywords = {LGM Pleistocene glaciation},
pages = {563 - 573},
publisher = {Elsevier},
series = {Developments in Quaternary Sciences},
timestamp = {2019-01-20T05:15:04.000+0100},
title = {{Pleistocene} Glaciation of {British} {Columbia}},
url = {http://www.sciencedirect.com/science/article/pii/B9780444534477000441},
volume = 15,
year = 2011
}