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Cordilleran ice sheet

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Cordilleran Ice Sheet
Map of North America during the Last Glacial Maximum, showing Cordilleran ice sheet (left) at maximum extent
Typecontinental
LocationNorth American Cordillera
Lowest elevationSea level
TerminusWest – Pacific Ocean
East – Great Plains
South – 40 degrees north latitude
Statusgone

The Cordilleran ice sheet was a major ice sheet that periodically covered large parts of North America during glacial periods over the last ~2.6 million years.

Extent

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The ice extent covered almost all of the continental shelf north of the Strait of Juan de Fuca and south from approximately the southwestern third of the Yukon Territory. This included all of mainland British Columbia, South Central Alaska, the Alaska Panhandle, and peninsula. The southern glacial maximums extended south to Washington state near Olympia in the west and to Spokane, the Idaho Panhandle, and much of Western Montana at the eastern glacial edge. At its eastern end the Cordilleran ice sheet merged with the Laurentide Ice Sheet at the Continental Divide, forming an area of ice that contained one and a half times as much water as the Antarctic ice sheet does today. The ice sheet faded north of the Alaska Range because the climate was too dry to form glaciers.[citation needed]

The ice sheet covered up to 2,500,000 km2 (970,000 sq mi) at the Last Glacial Maximum and probably more than that in some previous periods, when it may have extended into the northeast extremity of Oregon and the Salmon River Mountains in Idaho. It is probable, though, that its northern margin also migrated south due to the influence of starvation caused by very low levels of precipitation.[citation needed]

Refugia

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At its western end it is currently understood that several small glacial refugia existed during the last glacial maximum below present sea level in the now-submerged Hecate Strait and on the Brooks Peninsula in northern Vancouver Island. However, evidence of ice-free refugia above present sea level north of the Olympic Peninsula has been refuted by genetic and geological studies since the middle 1990s.

Thawing

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Unlike the Laurentide Ice Sheet, which may have taken as many as eleven thousand years to fully melt,[2] the Cordilleran ice sheet melted very quickly, probably in four thousand years or less.[3] This rapid melting caused floods such as the overflow of Lake Missoula and shaped the topography of the fertile Inland Empire of Eastern Washington.[4] Further north, the Cordilleran is responsible for a large number of glacial landforms scattered across the west of Canada.[5] The rate of thawing has also played a significant role in research surrounding early human migration into the American continents.

The rapid retreat of the Cordilleran ice sheet is a focus of study by glaciologists seeking to understand the difference in patterns of melting in marine-terminating glaciers, glaciers whose margin extends into open water without seafloor contact, and land-terminating glaciers, with a land or seafloor margin, as scientists believe the western marine-terminating margin retreated much faster than its southern, land-terminating front.[6] This rapid retreat resulted in noticeably fewer glacial landforms in the west of the Cordilleran's maximum extent compared to the south and east, though the exact mechanisms behind this disparity are unknown. Some glacial landforms are still present though: the well-characterized landscape of coastal Washington State contains glacial troughs, some glacial lakes, and an extensive outwash plain.[7] Many of the southern and eastern landforms fall near the northern reaches of the American Cordillera, the mountain ranges which geologists believe to be the region from which the Cordilleran first grew, and, after its sudden retreat and ultimate collapse, where it terminated.[8]

The timing of the retreat of the Cordilleran bears significance not just to glaciologists, but to anthropologists interested in the migration of early humans into the Americas. In particular, the collapse of the western front of the Cordilleran ice sheet has been proposed as one route through which early humans could have migrated after crossing the Beringian Land Bridge during the Last Glacial Maximum.[9] This serves as an alternative to the Ice Free Corridor previously posited to have allowed for migration amid the retreat of the eastern front of the Cordilleran ice sheet and the western front of the Laurentide ice sheet.[10] The Ice Free Corridor is a subject of debate among anthropologists in recent years. Recent studies have provoked skepticism, with areas of discussion including the lack of evidence of sufficient flora in the area to support megafaunal migration,[11] to radiometric dating placing the emergence of a corridor through the central Canadian Shield too late to account for the earliest known human sites south of the glaciers.[12]

Sea levels during glaciation

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Because of the weight of the ice, the mainland of northwest North America was so depressed that sea levels at the Last Glacial Maximum were over a hundred metres higher than they are today (measured by the level of bedrock).

However, on the western edge at the Haida Gwaii, the lower thickness of the ice sheet meant that sea levels were as much as 170 m (560 ft) lower than they are today, forming a lake in the deepest parts of the strait. This was because the much greater thickness of the center of the ice sheet served to push upwards areas at the edge of the continental shelf in a glacial forebulge. The effect of this during deglaciation was that sea levels on the edge of the ice sheet, which naturally deglaciated first, initially rose due to an increase in the volume of water, but later fell due to rebound after deglaciation. Some underwater features along the Pacific Northwest were exposed because of the lower sea levels, including Bowie Seamount west of Haida Gwaii which has been interpreted as an active volcanic island throughout the last ice age.

These effects are important because they have been used to explain how migrants to North America from Beringia were able to travel southward during the deglaciation process due purely to the exposure of submerged land between the mainland and numerous continental islands. They are also important for understanding the direction evolution has taken since the ice retreated.

See also

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References

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  1. ^ Fulton, R. J. & Prest, V. K. (1987). Introduction: The Laurentide Ice Sheet and its Significance. Géographie physique et Quaternaire, 41 (2), 181–186
  2. ^ Dyke, Arthur S. (2004), "An outline of North American deglaciation with emphasis on central and northern Canada", Quaternary Glaciations-Extent and Chronology - Part II: North America, Developments in Quaternary Sciences, vol. 2, Elsevier, pp. 373–424, doi:10.1016/s1571-0866(04)80209-4, ISBN 978-0-444-51592-6, retrieved 2024-04-01
  3. ^ Darvill, C. M.; Menounos, B.; Goehring, B. M.; Lesnek, A. J. (2022-05-28). "Cordilleran Ice Sheet Stability During the Last Deglaciation". Geophysical Research Letters. 49 (10). Bibcode:2022GeoRL..4997191D. doi:10.1029/2021GL097191. ISSN 0094-8276.
  4. ^ Topinka, L (2002). "The Cordilleran Ice Sheet and Missoula Floods". United States Geological Survey.
  5. ^ Arnold, H.; Ferbey, T.; Hickin, A. S. (2016). "Ice-flow indicator compilation, British Columbia and Yukon". ostrnrcan-dostrncan.canada.ca. doi:10.4095/298865. Retrieved 2024-03-08.
  6. ^ Lesnek, Alia J.; Briner, Jason P.; Baichtal, James F.; Lyles, Alex S. (July 2020). "New constraints on the last deglaciation of the Cordilleran Ice Sheet in coastal Southeast Alaska". Quaternary Research. 96: 140–160. Bibcode:2020QuRes..96..140L. doi:10.1017/qua.2020.32. ISSN 0033-5894.
  7. ^ Booth, Derek B.; Troost, Kathy Goetz; Clague, John J.; Waitt, Richard B. (2003), "The Cordilleran Ice Sheet", The Quaternary Period in the United States, vol. 1, Elsevier, pp. 17–43, Bibcode:2003DevQS...1...17B, doi:10.1016/s1571-0866(03)01002-9, ISBN 978-0-444-51470-7, retrieved 2024-04-01
  8. ^ Dulfer, Helen E.; Margold, Martin (2021-12-01). "Glacial geomorphology of the central sector of the Cordilleran Ice Sheet, Northern British Columbia, Canada". Journal of Maps. 17 (2): 413–427. Bibcode:2021JMaps..17..413D. doi:10.1080/17445647.2021.1937729. ISSN 1744-5647.
  9. ^ Lesnek, Alia J.; Briner, Jason P.; Lindqvist, Charlotte; Baichtal, James F.; Heaton, Timothy H. (2018-05-04). "Deglaciation of the Pacific coastal corridor directly preceded the human colonization of the Americas". Science Advances. 4 (5): eaar5040. Bibcode:2018SciA....4.5040L. doi:10.1126/sciadv.aar5040. ISSN 2375-2548. PMC 5976267. PMID 29854947.
  10. ^ Flannery, Tim F. (2002). The eternal frontier: an ecological history of North America and its peoples (2. [print.] ed.). New York, NY: Grove Press. ISBN 978-0-8021-3888-0.
  11. ^ Pedersen, Mikkel W.; Ruter, Anthony; Schweger, Charles; Friebe, Harvey; Staff, Richard A.; Kjeldsen, Kristian K.; Mendoza, Marie L. Z.; Beaudoin, Alwynne B.; Zutter, Cynthia; Larsen, Nicolaj K.; Potter, Ben A.; Nielsen, Rasmus; Rainville, Rebecca A.; Orlando, Ludovic; Meltzer, David J. (September 2016). "Postglacial viability and colonization in North America's ice-free corridor". Nature. 537 (7618): 45–49. Bibcode:2016Natur.537...45P. doi:10.1038/nature19085. ISSN 1476-4687. PMID 27509852.
  12. ^ Clark, Jorie; Carlson, Anders E.; Reyes, Alberto V.; Carlson, Elizabeth C. B.; Guillaume, Louise; Milne, Glenn A.; Tarasov, Lev; Caffee, Marc; Wilcken, Klaus; Rood, Dylan H. (2022-04-05). "The age of the opening of the Ice-Free Corridor and implications for the peopling of the Americas". Proceedings of the National Academy of Sciences. 119 (14): e2118558119. Bibcode:2022PNAS..11918558C. doi:10.1073/pnas.2118558119. ISSN 0027-8424. PMC 9168949. PMID 35312340.
  • Hidy, A. J., Gosse, J. C., Froese, D. G., Bond, J. D., and Rood, D. H. (2013). A latest Pliocene age for the earliest and most extensive Cordilleran Ice Sheet in northwestern Canada. Quaternary Science Reviews 61:77-84. [1]
  • Gwaii Haanas National Park Reserve and Haida Heritage Site[permanent dead link‍]
  • Clarke, T.E., D.B. Levin, D.H. Kavanaugh and T.E. Reimchen. 2001. Rapid Evolution in the Nebria Gregaria Group (Coleoptera: Carabidae) and the Paleogeography of the Queen Charlotte Islands. Evolution 51:1408–1418
  • Brown, A. S., and H. Nasmith. 1962. The glaciation of the Queen Charlotte Islands. Canadian Field-Naturalist 76:209–219.
  • Byun, S. A., B. F. Koop, and T. E. Reimchen. 1997. North American black bear mtDNA phylogeography: implications for morphology and the Haida Gwaii glacial refugium controversy. Evolution 51:1647–1653.
  • Richard B. Waitt, Jr., and Robert M. Thorson, 1983. The Cordilleran Ice Sheet in Washington, Idaho, and Montana. IN: H.E. Wright, Jr., (ed.), 1983, Late-Quaternary Environments of the United States, Volume 1: The Late Pleistocene (Stephen C. Porter (ed.)): University of Minnesota Press, 407p., Chapter 3, p.53-70. Abstract
  • Holder, K., Montgomerie, R., and V.L. Friesen. 1999. A test of the glacial refugium hypothesis using patterns of mitochondrial and nuclear DNA sequence variation in the rock ptarmingan (Lagopus mutus). Evolution 53(6):1936–1950. [2]
  • Warner, B.G., Mathewes, R.W., and J.J. Clague. 1982. Ice-free conditions on the Queen Charlotte Islands, British Columbia, at the height of late Wisconsin glaciation. Science 218(4573):675–6770 [3]


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