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Laurentide ice sheet
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{{short description|Continental glacier in North America during the last ice age}} {{Use dmy dates|date=April 2025}} {{Infobox glacier | child = | name = Laurentide ice sheet | other_name = | photo =Laurentide ice sheet map.jpg | photo_width = | photo_alt = | photo_caption =The maximum extent of North American ice sheets during the [[Last Glacial Maximum]] | map = <!-- or | map_image = --> | map_width = | map_alt = | map_caption = | type = Continental | location = [[North America]] | coordinates = | coords_ref = | area = | length = | width = | thickness = | elevation_max = {{ubl|Foxe-Baffin Dome: {{convert|2200|to|2400|m|ft}} above sea level|Keewatin Dome: {{convert|3200|m|ft}} above sea level<ref name=Lacelle2018>Lacelle, D.; Fisher, D. A.; Coulombe, S.; et al. (5 September 2018). "Buried remnants of the Laurentide Ice Sheet and connections to its surface elevation". ''Scientific Reports'' 8, 13286 (2018). {{doi|10.1038/s41598-018-31166-2}}.</ref>}} | elevation_min = Sea level | terminus = {{ubl|North – [[Arctic Ocean]]|East – [[Baffin Bay]]|South – 40 degrees north latitude|West – [[Rocky Mountains]]}} | status = Remnants: [[Barnes Ice Cap]], [[Penny Ice Cap]]<ref name=Lacelle2018/> | embedded = }} The '''Laurentide ice sheet''' (LIS) was a massive [[ice sheet|sheet of ice]] that covered millions of square miles, including most of [[Canada]] and a large portion of the [[Northern United States]], multiple times during the [[Quaternary glaciation]] epochs, from 2.58 million years ago to the present.<ref name="ICS StratChart 2022-02">{{cite web |title=Stratigraphic Chart 2022 |url=https://stratigraphy.org/ICSchart/ChronostratChart2022-02.pdf |publisher=International Stratigraphic Commission | date=February 2022 |access-date=4 June 2022}}</ref> The last advance covered most of northern North America between c. 95,000 and c. 20,000 years before the present day and, among other geomorphological effects, gouged out the five [[Great Lakes]] and the hosts of smaller lakes of the [[Canadian Shield]]. These lakes extend from the eastern [[Northwest Territories]], through most of northern Canada, and the upper [[Midwestern United States]] ([[Minnesota]], [[Wisconsin]], and [[Michigan]]) to the [[Finger Lakes]], through [[Lake Champlain]] and [[Lake George (lake), New York|Lake George]] areas of [[New York (state)|New York]], across the northern [[Appalachians]] into and through all of [[New England]] and [[Nova Scotia]]. At times, the ice sheet's southern margin included the present-day sites of coastal towns of the [[Northeastern United States]], and cities such as [[Boston]] and [[New York City]] and Great Lakes coastal cities and towns as far south as [[Chicago]] and [[St. Louis, Missouri]], and then followed the present course of the [[Missouri River]] up to the northern slopes of the [[Cypress Hills (Canada)|Cypress Hills]], beyond which it merged with the [[Cordilleran Ice Sheet]]. The ice coverage extended approximately as far south as 38 degrees latitude mid-continent.<ref name="dyke_prest">{{cite journal |last1=Dyke |first1=A. S. |last2=Prest |first2=V. K. |year=1987|title=Late Wisconsinan and Holocene History of the Laurentide Ice Sheet|journal=Géographie Physique et Quaternaire |volume=41 |issue=2 |pages=237–263 |doi=10.7202/032681ar |doi-access=}}</ref>
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